Striae Black & White Stock Photos
RF2B767FJ–Seperate starch grains, with striae and hilum, vintage line drawing or engraving illustration.
RM2WG0JBE–The International Exhibition: Bohemian glass, by Harrach of Bohemia, and Hofmann of Prague, in the Austrian Court, 1862. 'The central object...has its dishes and central column wrought of red glass cut into flat facets enriched with burnished gold...Both the large urn, or cup-shaped vessel, and the small vase in front of the dessert-dish, are in imitation malachite, the opaque striae and convolutions resulting from white glass being mingled with the dark green material of which they are formed...The elongated vase mounted on a pedestal...is formed of transparent green glass, which has been cov
RM2AKR17H–On Stratified Discharges.--IIObservations with a Revolving Mirror . the last. The elementary striae were, however, not so easilyseparable; and the flocculent striae were formed as usual at an earlierstage near the head of the column than near the foot of it. In another carbonic-acid tube the proper motion of the flocculent striaewas coincident in direction with that of the elementary; and the latterwere consequently more difficult to disentangle. One point in this tubewas particularly noticeable, viz. that as the column of flocculent striaeretreated, so did the negative glow advance. The two r
RF2AP2TWK–The black geometric head of zebra. Polygonal abstract animal of Africa. Vector illustration.
RF2B752H8–columnar cells found lining various parts of the intestines (called columnar epthelium), vintage line drawing or engraving illustration.
RF2MEJFN6–Close up of african pregnant woman holding her belly - Focus on hands - Black and white editing
RMPFXFBG–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ptycho. 840 immediately below the cardinal line ; separated from the body by a narrow but conspicuous depression. Surface ornamented by faint radiating striae which are obsolete except on perfectly preserved specimens, and also by fine concentric striae, which frequently become fasciculate on the anterior portion of the shell. This species may be distinguished from any other at present known by the slight obliqueness of the body of the shell, the basal margin
RF2CAB0PF–Woman smears nutritious cream sagging flabby belly with stretch marks, close-up, black and white photo.
RM2ANEMPT–The encyclopdia britannica; a dictionary of arts, sciences, literature and general information . —CCBEfiEL. OLf TUBER. PONS FLOC. From Cat. R.C.S. England. Fig. 20.—Mesial and Lateral Views of the Brain of Ornithorynchus. and back part of the ventricle, while the rudiments of the dorsalpart remain as the striae Jongitudinales on the corpus callosum.The dorsal part of the original anterior commissure beco^mes thefornix, and the paraterminal area is modified to form the septumlucidum. The first appearance of the fissure of Rolando is probablyin some of the Carnivora, in which, as the sulcus cruc
RMPFXFCF–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ptycho. 838 ating striae crossed by distinct concentric striae; resembles P.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lesley, J. P. (J. Peter), 1819-1903; Pennsylvania. Board of Commissioners for the Second Geological Survey. Harrisburg, Board of Commissioners for the Geological Su
RM2AKR0TY–On Stratified Discharges.--IIObservations with a Revolving Mirror . freer, it seems, the striae are to move. The same fact may be observedby comparing tubes differing in diameter, but in other respects thesame; but the conical tube brings out the fact in the most strikingmanner. Fig. 4 represents a chloroform-tube, in which a piece of cotton-woolhad been inserted with a view of ascertaining whether any motion wouldbe communicated to it by the current. This proved to be the case ; butI do not attempt here to describe the phenomenon. To the unassistedeye the discharge was extremely brilliant; it
RMPG2DBD–. The geological history of plants. Paleobotany; 1888. LAUEENTIAN AND EARLY PALAEOZOIC. 37 fronds smooth and slightly striate longitudinally, with curved and interrupted striae. Stem thick, bifurcating, the di-visions terminating in irregularly pinnate fronds, apparently truncate at the extremities. The quan- tity of carbona- ceous matter pres- entwonldindicate thick, though per- haps flattened, stems and dense fleshy fronds. The species Bufhotrephis sub- nodosa and B. flexuosa, from the Utica shale, are also certain- ly plants, though it, is possible, if their structures and fruit were known,
RM2ANENGC–The encyclopdia britannica; a dictionary of arts, sciences, literature and general information . 0LF:BULB{ COMM.V. PICR. L.. —CCBEfiEL. OLf TUBER. PONS FLOC. From Cat. R.C.S. England. Fig. 20.—Mesial and Lateral Views of the Brain of Ornithorynchus. and back part of the ventricle, while the rudiments of the dorsalpart remain as the striae Jongitudinales on the corpus callosum.The dorsal part of the original anterior commissure beco^mes thefornix, and the paraterminal area is modified to form the septumlucidum. The first appearance of the fissure of Rolando is probablyin some of the Carnivora,
RMPFYPR9–. Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 463 some of the markings usually to be seen in the cuticula are due to sense organs or to pores, most of them are inherent structural markings. These markings are used as specific, and in some cases as generic, characters. The cuticula of almost any species, if examined with sufficient care, will show transverse striations, ranging in the various species from a few score to upwards of a thousand. Many species described by earlier writers as destitute of these striations really possess them. When very fine the transverse striae ar
RM2AKR1PC–On Stratified Discharges.--IIObservations with a Revolving Mirror . traces a sketch of a flocculent stria. As the surface is stillfurther increased these diagonal lines appear more and more crowdedtogether, until at last they blend into unbroken flocculent striae. This confound nature and mode of formation may be taken as ageneral characteristic of the flocculent striae. In some tubes it is moreeasily brought out, in others only with greater difficulty. In some itcan hardly be verified experimentally without a loss of light so great asto mask the phenomenon. The apparent proper motion of the f
RMPFYPDY–. Fresh-water biology. Freshwater biology. THE WATER-MITES (HYDRACARINA) 853 or laterally, and in the males of certain species of Arrhenurus pro- longed posteriorly into a curious handle-like appendage. The form is more definite in the higher forms than in those which seem most primitive. The skin in some forms is soft and the surface smooth, but more usually it is marked by fine striae like the lines on the palm of the hand, and in the lower forms it is often granulated or papillated. Other species possess chitinous plates, which may be few and small or larger and more numerous, and may even
RM2AWEN4Y–Clinical and pathological papers .. . Fig. 2.—Showing the strite about the knees. those on the left, making a total of forty-two. The positions ofthese striae are seen in the accompanying pictures (Figs. 2 and 3).They were a delicate pink color, in marked contrast to the surround-ing skin, and were painless, causing the patient no inconveniencewhatever. There were no sensory disturbances in this case. Dur-ing the patients prolonged stay in bed he grew about four inches inheight, and it seems to me that the most reasonable explanation of thestriae is the stretching of the skin from the rapid gr
RMPFXYBJ–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ind.1881. Hall,28th Rt., 1876 ; Fenestella ambigua, Hall, 28th Rt., 1879). CoUett's Indiana Report of 1881, page 248, plate 10, figs.p? to 21. In well-preserved specimens there are rows of minute pits between the striae.—Niagara, Vb. lionchocephalus chippewaensis (Conccephalus chippe-. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations ma
RM2AJEFG3–Report on paleontology . ata Mort. sp. (p. 177). 1<^1G8. 1, 2. Views of the opposite sides of a large specimen showing the general features. 3. Basal view of the same specimen showing the character of the umbilical cavity and the flattened callosity around it. Acad. Nat. Sci., Phila. 4. Enlargement of four of tlie ribs from the body volution. 5. A further enlargement of one rib to show the finer vertical striae. Plelrotomaria Tintonknsis Whitf. (p. 178). 7-9. Vertical, basal, front and lateral views of the specimen described, which I am inclined tothink is a European specimen. Collection at
RMPG43JX–. The anatomy of the common squid, Loligo pealii, Lesueur. Squids; Mollusks. 31 cutting edge of the jaw. This edge is drawn up into a strong median tooth which is flanked by a pair of small notches. The pharyngeal muscles are attach- ed to the adjacent surfaces of the lamellae of each jaw and fill the narrow space between them. The jaws grow constantly by additions to their margin's and to their unexposed surfaces. They are marked by two sets of fine striae, the lines of growth, one set concentric with the point of the jaw and one set radiating from it. The jaws are brown- ish-black on the cut
RM2AND31K–The Silver VoltameterPart IPart II . d, in consequence, for thesame current density striae were produced in the Rayleigh form when they wereabsent in the Richards form. This effect has also been observed by Guthe# and byYAK DiJKf. In the Richards form, as employed by the latter observer, the kathode * Guthe, <Phys. Key./ 19, p. 147, 1904. t VAN Dijk, Ann. der Phys., 19, p. 271, 1906. ON THE SILVER VOLTAMETER. 577 liquid consisted of about 30 cub. centims. of a 20 per cent, solution, and at timesnearly 3 grammes of silver were deposited, the concentration being thus reduced toabout 43 per ce
![. The Eurypterida of New York. Eurypterida; Paleontology. 348 NEW YORK STATE MUSEUM This is the first stage in which the fine transverse sculpture lines could be recognized [pi. 64, fig. 5]. Horizon and locality. This species is one of the most common forms in the fauna of the Shawangunk grit at Otisville, N. Y. Remarks. H. shawangunk differs from the genot3^pe in its smaller size, somewhat broader carapace and most distinctly in the surface sculpture which is characterized by parallel, transverse striae, absent in the other species. Genus PTERYGOTUS Agassiz Pterygotus will always be historica Stock Photo](https://c8.alamy.com/comp/PFY1T2/the-eurypterida-of-new-york-eurypterida-paleontology-348-new-york-state-museum-this-is-the-first-stage-in-which-the-fine-transverse-sculpture-lines-could-be-recognized-pi-64-fig-5-horizon-and-locality-this-species-is-one-of-the-most-common-forms-in-the-fauna-of-the-shawangunk-grit-at-otisville-n-y-remarks-h-shawangunk-differs-from-the-genot3pe-in-its-smaller-size-somewhat-broader-carapace-and-most-distinctly-in-the-surface-sculpture-which-is-characterized-by-parallel-transverse-striae-absent-in-the-other-species-genus-pterygotus-agassiz-pterygotus-will-always-be-historica-PFY1T2.jpg ". The Eurypterida of New York. Eurypterida; Paleontology. 348 NEW YORK STATE MUSEUM This is the first stage in which the fine transverse sculpture lines could be recognized [pi. 64, fig. 5]. Horizon and locality. This species is one of the most common forms in the fauna of the Shawangunk grit at Otisville, N. Y. Remarks. H. shawangunk differs from the genot3^pe in its smaller size, somewhat broader carapace and most distinctly in the surface sculpture which is characterized by parallel, transverse striae, absent in the other species. Genus PTERYGOTUS Agassiz Pterygotus will always be historica Stock Photo")
RMPFY1T2–. The Eurypterida of New York. Eurypterida; Paleontology. 348 NEW YORK STATE MUSEUM This is the first stage in which the fine transverse sculpture lines could be recognized [pi. 64, fig. 5]. Horizon and locality. This species is one of the most common forms in the fauna of the Shawangunk grit at Otisville, N. Y. Remarks. H. shawangunk differs from the genot3^pe in its smaller size, somewhat broader carapace and most distinctly in the surface sculpture which is characterized by parallel, transverse striae, absent in the other species. Genus PTERYGOTUS Agassiz Pterygotus will always be historica
RM2AWEPFH–Clinical and pathological papers .. . e leg there were in allnineteen of these scars, irregularly placed, the lowest being on a H Typhoid Fever and Other Exanthemata, second edition, 1909, p. 177.56 Johns Hopkins Hosp. Bull, v, 19. Digitized by Microsoft® PHILLIPS: SKIN RASHES IN TYPHOID FEVER 9 level with the tip of the internal malleolus, the highest 14.5 cm.above this point. They lay transversely, and varied in length from1 cm. to 3 cm. The average width of the striae was 9 cm. Directlyover the centre of the patella, and extending transversely, was oneof these striae, 2.5 cm. in length, 0.2
RMPFXJ1M–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 233, plate 78 B^ fig. 2, a portion of Hall's complete figure, show- ing only the inhabited chamber, and the three narrow chambers behind it, eight others to the smaller end being cut off; also the open end of the large chamber cut ofi*. The scratches (striae) on one part of the surface are bent to a middle line, not because this is their natural mode of appearance, but the animal thus repaired some violent fracture of its shell, which was thereby thickened an
RM2AJEGPY–Report on paleontology . ont and back views of a very large specimen from Crosswicks, in the Columbia Collegecollection.9. View of a smaller specimen. Collection Acad. Nat. Sci., Phila. Cyhchna kecta Gabb (p. 164). 10, H. Two views of the type specimen enlarged two diameters. Dentauum (Falcdla) falcatum Conrad (p. 169). 12,14. View of stnaU much curved specimen, all casts.15-17. Views of the larger portion of three individual oasts. 16. Portion of a partial cast, looking on the back and showing striae of growth. Acad. Nat.Sci. Phila. Dentalium subarcuatum Conrad (p. 166). 19. View of a crushed
![. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. LUNUL. 364 liunulicardium ornatum {Pinnopsis ornatus). Hall, Keport on the Third or Western ^"'*^' ^^'^ District of New York, 1843, page 106^ /j^B^^^S^ y^licardium acutirostra (which lived with it in the same Portage sandstone formation) that they are often mistaken for each other; but this has more than 40 diverg- ing ribs, and the other only 26; and they are crossed by beauti- fully arched striae. The general shape of the two shells differs also.—Casha Stock Photo](https://c8.alamy.com/comp/PFXY7P/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-lunul-364-liunulicardium-ornatum-pinnopsis-ornatus-hall-keport-on-the-third-or-western-quot-district-of-new-york-1843-page-106-jbs-ylicardium-acutirostra-which-lived-with-it-in-the-same-portage-sandstone-formation-that-they-are-often-mistaken-for-each-other-but-this-has-more-than-40-diverg-ing-ribs-and-the-other-only-26-and-they-are-crossed-by-beauti-fully-arched-striae-the-general-shape-of-the-two-shells-differs-alsocasha-PFXY7P.jpg ". A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. LUNUL. 364 liunulicardium ornatum {Pinnopsis ornatus). Hall, Keport on the Third or Western ^"'*^' ^^'^ District of New York, 1843, page 106^ /j^B^^^S^ y^licardium acutirostra (which lived with it in the same Portage sandstone formation) that they are often mistaken for each other; but this has more than 40 diverg- ing ribs, and the other only 26; and they are crossed by beauti- fully arched striae. The general shape of the two shells differs also.—Casha Stock Photo")
RMPFXY7P–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. LUNUL. 364 liunulicardium ornatum {Pinnopsis ornatus). Hall, Keport on the Third or Western ^"'*^' ^^'^ District of New York, 1843, page 106^ /j^B^^^S^ y^licardium acutirostra (which lived with it in the same Portage sandstone formation) that they are often mistaken for each other; but this has more than 40 diverg- ing ribs, and the other only 26; and they are crossed by beauti- fully arched striae. The general shape of the two shells differs also.—Casha
RMRDT2B8–. Principles of economic zoo?logy. Zoology, Economic. INSECTA 117 chemical composition; or physical, depending upon the structural or physical make-up; or it may be due to a combination of both of these. In the most highly colored group of insects, the Lepidoptera, the color is due to the chemical substances (pigment granules), to the structural character of the scale. Fig. 90.—The protective resemblance of the leaf-butterfly (Kal'lima). (Holder, after Wallace.) walls (striae), and to the overlapping (lamination) of the scales laterally, as well as to the overlapping of the tips of the scales
RMPG3HGY–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE STAG BEETLES. 907 bles with a large median tooth which points obliquely inward and upward. Elytra deeply striate, both striae and intervals finely and rather closely punctured. Length 15-26 mm. Throughout the State; frequent. April 27-December 8. Hi- bernates beneath old, partly burned logs. Occurs most commonly in June and July about the roots of oak, linn and maple trees and stumps, in the decaying woo
![. The physiology of reproduction. Reproduction. 362 THE PHYSIOLOGY OF REPRODUCTION disappear at parts. The nuclei are numerous, and most of the authorities agree on the absence of mitoses, some holding that they divide directly, others that they have lost the power of division. The protoplasm has a foam-hke structure, and in Man it is condensed superficially to form a layer which bears the " Biirstenbesatz " or striated border (Fig. 75). This consists, as seen in fixed specimens, of a series of fine striae running per- pendicularly to the surface, and its structure and function have Stock Photo](https://c8.alamy.com/comp/RE1CT1/the-physiology-of-reproduction-reproduction-362-the-physiology-of-reproduction-disappear-at-parts-the-nuclei-are-numerous-and-most-of-the-authorities-agree-on-the-absence-of-mitoses-some-holding-that-they-divide-directly-others-that-they-have-lost-the-power-of-division-the-protoplasm-has-a-foam-hke-structure-and-in-man-it-is-condensed-superficially-to-form-a-layer-which-bears-the-quot-biirstenbesatz-quot-or-striated-border-fig-75-this-consists-as-seen-in-fixed-specimens-of-a-series-of-fine-striae-running-per-pendicularly-to-the-surface-and-its-structure-and-function-have-RE1CT1.jpg ". The physiology of reproduction. Reproduction. 362 THE PHYSIOLOGY OF REPRODUCTION disappear at parts. The nuclei are numerous, and most of the authorities agree on the absence of mitoses, some holding that they divide directly, others that they have lost the power of division. The protoplasm has a foam-hke structure, and in Man it is condensed superficially to form a layer which bears the " Biirstenbesatz " or striated border (Fig. 75). This consists, as seen in fixed specimens, of a series of fine striae running per- pendicularly to the surface, and its structure and function have Stock Photo")
RMRE1CT1–. The physiology of reproduction. Reproduction. 362 THE PHYSIOLOGY OF REPRODUCTION disappear at parts. The nuclei are numerous, and most of the authorities agree on the absence of mitoses, some holding that they divide directly, others that they have lost the power of division. The protoplasm has a foam-hke structure, and in Man it is condensed superficially to form a layer which bears the " Biirstenbesatz " or striated border (Fig. 75). This consists, as seen in fixed specimens, of a series of fine striae running per- pendicularly to the surface, and its structure and function have
RMPG3WHH–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE GROUND BEETLES. 57 dd. Strife not extending to base of elytra; tip of elytra rufous. .'/. Elytral strijie strongly punctate; thorax ovate, broader than long. 54. H.EMOKRHOIDALIS. !JU- Elytral striae feebly punctate; thorax quadrate-globose. 55. TEEIIINATUS. hh. Third interval of elytra with two punctures or none at all. U. Aiiical spur of front tibkc very short; elytral strire coarsely punc- tured, alise
RMRDJF0J–. The doctrine of descent and Darwinism. Evolution. TYPE OF DEVELOPMENT OF ARTICULATA. S3 rounded itself with a germinal membrane, a portion of it thickens into a long germinal stria, resembling an elon- gated ellipse. This is the rudiment of the ventral side of the future animal. A groove then divides it into the two germinal laminae, and transverse striae next make their appearance, the indications of the so-called primordial segments. The symmetrical disposition of the organs, and the integration of the body out of consecutive segments, is herewith initiated. All further development emanate
RMPFYMAR–. Fresh-water biology. Freshwater biology. S4 (so) Valves asymmetrical with reference to a transverse axis. Family Meridionaceae. Only one genus Meridian Agardh. Both valve and girdle sides wedge-shaped, forming ring- like or fan-shaped bands; striations uninterrupted. There are imperfect transverse septa which are con- spicuous on the valve side but show only laterally on the girdle side. Between these on the valve side are fine punctate striae. Van Heurck thinks this genus ought to be suppressed. It differs from Dialoma only in the cuneate shape of the valves.. Fig. 98. Meridion constriclum
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an Stock Photo](https://c8.alamy.com/comp/RJ5KEB/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-600-the-upper-silurian-i-the-trenton-limestone-but-a-careful-comparison-shows-it-to-be-wider-and-more-abrupt-at-its-posterior-termination-while-the-direction-of-the-striae-of-growth-is-very-distinctive-these-marks-being-regularly-curving-toward-the-posterior-end-in-m-nasutus-while-in-this-species-they-are-abruptly-bent-at-the-postero-basal-angle-an-RJ5KEB.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an Stock Photo")
RMRJ5KEB–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an
![. Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 495 46 (45) Pharynx not long and narrow 47 47 (48) Striae not resolvable into rows of dots Cephalobus Bastian. Genus of numerous species, frequent about the higher plants, doubtless often at least "semi- parasitic." Occasionally species in fresh water. Common in decaying vegetable matter. Some species are parthenogenetic, others hermaphroditic. Found on the surface of insects. Cephalobus resembles Rhabdilis, but may readily be distinguished by the form of the pharynx and the nature of the male caudal armature. The phar Stock Photo](https://c8.alamy.com/comp/PFYJNT/fresh-water-biology-freshwater-biology-free-living-nematodes-495-46-45-pharynx-not-long-and-narrow-47-47-48-striae-not-resolvable-into-rows-of-dots-cephalobus-bastian-genus-of-numerous-species-frequent-about-the-higher-plants-doubtless-often-at-least-quotsemi-parasiticquot-occasionally-species-in-fresh-water-common-in-decaying-vegetable-matter-some-species-are-parthenogenetic-others-hermaphroditic-found-on-the-surface-of-insects-cephalobus-resembles-rhabdilis-but-may-readily-be-distinguished-by-the-form-of-the-pharynx-and-the-nature-of-the-male-caudal-armature-the-phar-PFYJNT.jpg ". Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 495 46 (45) Pharynx not long and narrow 47 47 (48) Striae not resolvable into rows of dots Cephalobus Bastian. Genus of numerous species, frequent about the higher plants, doubtless often at least "semi- parasitic." Occasionally species in fresh water. Common in decaying vegetable matter. Some species are parthenogenetic, others hermaphroditic. Found on the surface of insects. Cephalobus resembles Rhabdilis, but may readily be distinguished by the form of the pharynx and the nature of the male caudal armature. The phar Stock Photo")
RMPFYJNT–. Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 495 46 (45) Pharynx not long and narrow 47 47 (48) Striae not resolvable into rows of dots Cephalobus Bastian. Genus of numerous species, frequent about the higher plants, doubtless often at least "semi- parasitic." Occasionally species in fresh water. Common in decaying vegetable matter. Some species are parthenogenetic, others hermaphroditic. Found on the surface of insects. Cephalobus resembles Rhabdilis, but may readily be distinguished by the form of the pharynx and the nature of the male caudal armature. The phar
RMRDJ5PF–. The doctrine of descent and Darwinism. Evolution. TYPE OF DEVELOPMENT OF ARTICULATA. S3 rounded itself with a germinal membrane, a portion of it thickens into a long germinal stria, resembling an elon- gated ellipse. This is the rudiment of the ventral side of the future animal. A groove then divides it into the two germinal laminae, and transverse striae next make their appearance, the indications of the so-called primordial segments. The symmetrical disposition of the organs, and the integration of the body out of consecutive segments, is herewith initiated. All further development emanate
RMPFXGG6–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 1862,page 50,plate 4,fig. 12. — Upper Heldevlerg for- mation^ VIII a. Concen- tric striae on the surface ^r^m^^ .. raised in little bundles (f as- Piall/S^' ^^'^' cicles), bending backward gently from the sutare,reach the flattened spiral band. This shell, living with M. maia, and M, leda, differs by its greater length of volutions and flattening on the upper side. Upper Held- Corniferous limestone at the falls of the Ohio. Probably some of the many New'York
RMRD7K3W–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ptycho. 840 immediately below the cardinal line ; separated from the body by a narrow but conspicuous depression. Surface ornamented by faint radiating striae which are obsolete except on perfectly preserved specimens, and also by fine concentric striae, which frequently become fasciculate on the anterior portion of the shell. This species may be distinguished from any other at present known by the slight obliqueness of the body of the shell, the basal margin
![. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. (Hall,35th An. Rt. Mus. 1882.) Oollett's Indian Rt., 1882, page 303, plate 27; figs. 7,8.— Falls of Ohio, Corniferous limestone.— Villa. The genus is Lonsdale's. Hall's description of the spe- cies on page 458 of the 35th An. Rt. is as follows: " Oor- allum sub-cylindrical, simple or compound, increasing by lateral gemmation, fre- quently in contact for their entire length; exterior with very regular annulations and concentric striae; longitudinal striae Stock Photo](https://c8.alamy.com/comp/PFXJ7E/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-hall35th-an-rt-mus-1882-oolletts-indian-rt-1882-page-303-plate-27-figs-78-falls-of-ohio-corniferous-limestone-villa-the-genus-is-lonsdales-halls-description-of-the-spe-cies-on-page-458-of-the-35th-an-rt-is-as-follows-quot-oor-allum-sub-cylindrical-simple-or-compound-increasing-by-lateral-gemmation-fre-quently-in-contact-for-their-entire-length-exterior-with-very-regular-annulations-and-concentric-striae-longitudinal-striae-PFXJ7E.jpg ". A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. (Hall,35th An. Rt. Mus. 1882.) Oollett's Indian Rt., 1882, page 303, plate 27; figs. 7,8.— Falls of Ohio, Corniferous limestone.— Villa. The genus is Lonsdale's. Hall's description of the spe- cies on page 458 of the 35th An. Rt. is as follows: " Oor- allum sub-cylindrical, simple or compound, increasing by lateral gemmation, fre- quently in contact for their entire length; exterior with very regular annulations and concentric striae; longitudinal striae Stock Photo")
RMPFXJ7E–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. (Hall,35th An. Rt. Mus. 1882.) Oollett's Indian Rt., 1882, page 303, plate 27; figs. 7,8.— Falls of Ohio, Corniferous limestone.— Villa. The genus is Lonsdale's. Hall's description of the spe- cies on page 458 of the 35th An. Rt. is as follows: " Oor- allum sub-cylindrical, simple or compound, increasing by lateral gemmation, fre- quently in contact for their entire length; exterior with very regular annulations and concentric striae; longitudinal striae
RMRDAXC8–. Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 463 some of the markings usually to be seen in the cuticula are due to sense organs or to pores, most of them are inherent structural markings. These markings are used as specific, and in some cases as generic, characters. The cuticula of almost any species, if examined with sufficient care, will show transverse striations, ranging in the various species from a few score to upwards of a thousand. Many species described by earlier writers as destitute of these striations really possess them. When very fine the transverse striae ar
RMPFYJNK–. Fresh-water biology. Freshwater biology. 496 FRESH-WATER BIOLOGY 48 (47) Striae resolvable into rows of dots, altered on lateral fields. Teratocephalus de Man. Interesting genus of tew species, with movable cuticular lips. Species have thus far been found only in fresh water and wet soils, but the genus appears to have a world-wide distribution, at least in temperate regions. Teratocephalus seems related to Cephalobus from which, how- ever, it differs strikingly in the formation of the lips and pharynx. It is difficult to determine the functions of the movable cuticular labial elements (a).
RMRDF2P8–. The geological history of plants. Paleobotany; 1888. LAUEENTIAN AND EARLY PALAEOZOIC. 37 fronds smooth and slightly striate longitudinally, with curved and interrupted striae. Stem thick, bifurcating, the di-visions terminating in irregularly pinnate fronds, apparently truncate at the extremities. The quan- tity of carbona- ceous matter pres- entwonldindicate thick, though per- haps flattened, stems and dense fleshy fronds. The species Bufhotrephis sub- nodosa and B. flexuosa, from the Utica shale, are also certain- ly plants, though it, is possible, if their structures and fruit were known,
![. The book of the garden. Gardening. YELLOW-BOOTED B£AN BEETLE.. O, WIRE-WORM; &, CAUDAL JOINT MAGNIFIED ; C, PERFECT BEETLE ; d, ANTENNA. third of an inch in length, and is described by Stephens as being " foscous, with a griseoua pubescence. Head and thorax blackish, the latter with the lateral branches nearly straight, and the posterior angles very acute; the disc very convex, and thickly punctate; scutellum fuscous; elytra broad, a little attenuated, round- ed at the apex, very convex; punctate striated; the striae disposed in pairs, and united at the apex, griseous yellow, with t Stock Photo](https://c8.alamy.com/comp/PG3FB6/the-book-of-the-garden-gardening-yellow-booted-ban-beetle-o-wire-worm-amp-caudal-joint-magnified-c-perfect-beetle-d-antenna-third-of-an-inch-in-length-and-is-described-by-stephens-as-being-quot-foscous-with-a-griseoua-pubescence-head-and-thorax-blackish-the-latter-with-the-lateral-branches-nearly-straight-and-the-posterior-angles-very-acute-the-disc-very-convex-and-thickly-punctate-scutellum-fuscous-elytra-broad-a-little-attenuated-round-ed-at-the-apex-very-convex-punctate-striated-the-striae-disposed-in-pairs-and-united-at-the-apex-griseous-yellow-with-t-PG3FB6.jpg ". The book of the garden. Gardening. YELLOW-BOOTED B£AN BEETLE.. O, WIRE-WORM; &, CAUDAL JOINT MAGNIFIED ; C, PERFECT BEETLE ; d, ANTENNA. third of an inch in length, and is described by Stephens as being " foscous, with a griseoua pubescence. Head and thorax blackish, the latter with the lateral branches nearly straight, and the posterior angles very acute; the disc very convex, and thickly punctate; scutellum fuscous; elytra broad, a little attenuated, round- ed at the apex, very convex; punctate striated; the striae disposed in pairs, and united at the apex, griseous yellow, with t Stock Photo")
RMPG3FB6–. The book of the garden. Gardening. YELLOW-BOOTED B£AN BEETLE.. O, WIRE-WORM; &, CAUDAL JOINT MAGNIFIED ; C, PERFECT BEETLE ; d, ANTENNA. third of an inch in length, and is described by Stephens as being " foscous, with a griseoua pubescence. Head and thorax blackish, the latter with the lateral branches nearly straight, and the posterior angles very acute; the disc very convex, and thickly punctate; scutellum fuscous; elytra broad, a little attenuated, round- ed at the apex, very convex; punctate striated; the striae disposed in pairs, and united at the apex, griseous yellow, with t
RMRDY5KE–. The anatomy of the domestic animals . Veterinary anatomy. ndge formed by the junction of the frog with the bar and sole. This surface presents fine striae and openings for the papillae of the corium. The external or grotand surface presents a central sulcus (Sulcus cunei), which is bounded by two ridges or crura (Crura cunei). The medial and lat- eral surfaces (Facies medialis et lat- eralis) are united at the upper part with the bars and sole, but are free below and form the central wall of the deep collateral sulci (Sulci para- cuneati), which are bounded out- wardly by the bars. The base
RMPFTTXW–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 10th Regents Rt. 1857. Chemung,) Hall, Pal.N. Y. Vol. IV, 1867, page 170, plate 24, figs. 1 to 9. It occurs in the same beds with P. loydii and P. hirsuta^ but is easily distinguished from them by its greater gibbosity and fewer spines; and its casts, by extremely fine papillas and their extension in hairlike striae. In general characters it resembles P. suhalataoH the Hamilton formation^ in Illinois. Found in the ChemunghedsdX Phillips- burg, Alleghany Co.,
RMRDXNWP–. The anatomy of the domestic animals . Veterinary anatomy. 788 NERVOUS SYSTEM OF THE HOHSE olfactorii) which is connected with the lateral ventricle by a small canal in the olfactory tract. The deep face is largely in contact with the frontal pole of the hemisphere and is connected with the olfactory tract. The gray matter of the bulb is external and is tliickest on the convex anterior surface. The posterior part consists to a large extent of fibers which are the axones of the mitral oeUs of the deep layer of the gray substance and go to form the tract and striae. The olfactory tract (Tractus
RMPG3WGD–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. lOS FAMILY IT. CAEABin.+;. ee. Sides of thorax not flattened; prosternum without setae; piceous. shining. 166. chalcea. dd. Prostenmm of male smooth as in the females and without setse; sides of thorax not flattened. ^ /'. Elytral striae fine, the intervals flat; thorax distinctly emarginate at apex. 167. sub^nea. ff. Elytral strife deep, the intervals convex: thorax nearly trimcate at apex. g. Foim oblnng;
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s Stock Photo](https://c8.alamy.com/comp/RJ5KE4/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-i-the-trenton-limestone-but-a-careful-comparison-shows-it-to-be-wider-and-more-abrupt-at-its-posterior-termination-while-the-direction-of-the-striae-of-growth-is-very-distinctive-these-marks-being-regularly-curving-toward-the-posterior-end-in-m-nasutus-while-in-this-species-they-are-abruptly-bent-at-the-postero-basal-angle-and-again-on-the-cardinal-s-RJ5KE4.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s Stock Photo")
RMRJ5KE4–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s
RMPFW0C0–. Fresh-water biology. Freshwater biology. 0.1 MM. 45 (40) Valves obscurely reticulated and with some striae. Posterior and ventral margins straight, the latter extended into a point or spine. . , Scapholeheris Schoedler 1858 . 46 Body not compressed; shape more or less quadrate. Cervical sinus deep. Fornices and rostrum well developed. Head small, depressed. Valves almost rectangular, the infero- posteal angle of each produced into a longer or shorter spine; ventral margin with short, fine setae. Claws denticulate, not pectinate. One abdominal projection developed. Antennules small, about ali
RMRD7K5D–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ptycho. 838 ating striae crossed by distinct concentric striae; resembles P.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lesley, J. P. (J. Peter), 1819-1903; Pennsylvania. Board of Commissioners for the Second Geological Survey. Harrisburg, Board of Commissioners for the Geological Su
RMPFXER5–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. page 238, plate 43, figs. 1 a, J, c?, d, back, belly, side, front of specimen of ordinary size and proportion; e, /*, ^, A, of a more pot-bellied (ventricose) specimen; ^, A, of an extreme case; Z, one longer than usual; m, enlarged^ plications showing im- pressed lines and strong striae in the front of the shell. Belongs to the type of R, wilsoni and is one of the forms often re- ferred to that species. In some of its variations it resembles E. pyramidata ;
![. The Eurypterida of New York. Eurypterida; Paleontology. 348 NEW YORK STATE MUSEUM This is the first stage in which the fine transverse sculpture lines could be recognized [pi. 64, fig. 5]. Horizon and locality. This species is one of the most common forms in the fauna of the Shawangunk grit at Otisville, N. Y. Remarks. H. shawangunk differs from the genot3^pe in its smaller size, somewhat broader carapace and most distinctly in the surface sculpture which is characterized by parallel, transverse striae, absent in the other species. Genus PTERYGOTUS Agassiz Pterygotus will always be historica Stock Photo](https://c8.alamy.com/comp/RD7THR/the-eurypterida-of-new-york-eurypterida-paleontology-348-new-york-state-museum-this-is-the-first-stage-in-which-the-fine-transverse-sculpture-lines-could-be-recognized-pi-64-fig-5-horizon-and-locality-this-species-is-one-of-the-most-common-forms-in-the-fauna-of-the-shawangunk-grit-at-otisville-n-y-remarks-h-shawangunk-differs-from-the-genot3pe-in-its-smaller-size-somewhat-broader-carapace-and-most-distinctly-in-the-surface-sculpture-which-is-characterized-by-parallel-transverse-striae-absent-in-the-other-species-genus-pterygotus-agassiz-pterygotus-will-always-be-historica-RD7THR.jpg ". The Eurypterida of New York. Eurypterida; Paleontology. 348 NEW YORK STATE MUSEUM This is the first stage in which the fine transverse sculpture lines could be recognized [pi. 64, fig. 5]. Horizon and locality. This species is one of the most common forms in the fauna of the Shawangunk grit at Otisville, N. Y. Remarks. H. shawangunk differs from the genot3^pe in its smaller size, somewhat broader carapace and most distinctly in the surface sculpture which is characterized by parallel, transverse striae, absent in the other species. Genus PTERYGOTUS Agassiz Pterygotus will always be historica Stock Photo")
RMRD7THR–. The Eurypterida of New York. Eurypterida; Paleontology. 348 NEW YORK STATE MUSEUM This is the first stage in which the fine transverse sculpture lines could be recognized [pi. 64, fig. 5]. Horizon and locality. This species is one of the most common forms in the fauna of the Shawangunk grit at Otisville, N. Y. Remarks. H. shawangunk differs from the genot3^pe in its smaller size, somewhat broader carapace and most distinctly in the surface sculpture which is characterized by parallel, transverse striae, absent in the other species. Genus PTERYGOTUS Agassiz Pterygotus will always be historica
RMPG3HRM–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE CLICK BEETLES. 741 1397 (4281). Agriotes insanus Cand., Blat, IV, 376. Elongate-oblong; slender, convex. Pale dull brown; head and thorax somewhat darker; legs paler. Thorax slightly longer than broad; sides rounded on apical third; hind angles feebly diverging, subacute, not visibly earinate; disk with a median impressed line on basal half, rather densely and finely punctate. Elytral striae rather finel
RMRE9NPB–. Contributions from the Botanical Laboratory, vol. 8. Botany; Botany. Fig. Cellulose (parallel lines, upper right), protoplasm (broken lines, lower left), and nucleus (spotted circle) of living onion cell (nucleus is 20/i across). other with only occasional irregularities. The general arrangement of the striae is often strikingly symmetrical (Figs. 7 and 8). At times, the striae run at right angles to or even cut diagonally across each other. There is little difference to be seen in the ultramicroscopic structure of the epidermal walls of elder, onion, and celery, nor does it matter (as regar
RMPFXHHN–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Goniatites bicostatus. Hall, Geology of the Fourth or Western District of New York, 1843, page 245, vlll.'L«8S8g9,M. gg 207, 8 ; marked by an elevated line on each side of the back ; the arched striae, rising from the umbilicus, meet this line at an acute for- ward angle, and recede from it at a still acuter ' angle, to ride over the back. Shore of Lake Erie, Chatauqua Co., N. Y., in Portage strata^ VIII f. Goniatites chemungensis. Vanuxem, Geology of the mil
![. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. LUNUL. 364 liunulicardium ornatum {Pinnopsis ornatus). Hall, Keport on the Third or Western ^"'*^' ^^'^ District of New York, 1843, page 106^ /j^B^^^S^ y^licardium acutirostra (which lived with it in the same Portage sandstone formation) that they are often mistaken for each other; but this has more than 40 diverg- ing ribs, and the other only 26; and they are crossed by beauti- fully arched striae. The general shape of the two shells differs also.—Casha Stock Photo](https://c8.alamy.com/comp/RD7NA9/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-lunul-364-liunulicardium-ornatum-pinnopsis-ornatus-hall-keport-on-the-third-or-western-quot-district-of-new-york-1843-page-106-jbs-ylicardium-acutirostra-which-lived-with-it-in-the-same-portage-sandstone-formation-that-they-are-often-mistaken-for-each-other-but-this-has-more-than-40-diverg-ing-ribs-and-the-other-only-26-and-they-are-crossed-by-beauti-fully-arched-striae-the-general-shape-of-the-two-shells-differs-alsocasha-RD7NA9.jpg ". A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. LUNUL. 364 liunulicardium ornatum {Pinnopsis ornatus). Hall, Keport on the Third or Western ^"'*^' ^^'^ District of New York, 1843, page 106^ /j^B^^^S^ y^licardium acutirostra (which lived with it in the same Portage sandstone formation) that they are often mistaken for each other; but this has more than 40 diverg- ing ribs, and the other only 26; and they are crossed by beauti- fully arched striae. The general shape of the two shells differs also.—Casha Stock Photo")
RMRD7NA9–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. LUNUL. 364 liunulicardium ornatum {Pinnopsis ornatus). Hall, Keport on the Third or Western ^"'*^' ^^'^ District of New York, 1843, page 106^ /j^B^^^S^ y^licardium acutirostra (which lived with it in the same Portage sandstone formation) that they are often mistaken for each other; but this has more than 40 diverg- ing ribs, and the other only 26; and they are crossed by beauti- fully arched striae. The general shape of the two shells differs also.—Casha
RMPFXHHT–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 255 GONI.. Goniatites bicostatus. Hall, Geology of the Fourth or Western District of New York, 1843, page 245, vlll.'L«8S8g9,M. gg 207, 8 ; marked by an elevated line on each side of the back ; the arched striae, rising from the umbilicus, meet this line at an acute for- ward angle, and recede from it at a still acuter ' angle, to ride over the back. Shore of Lake Erie, Chatauqua Co., N. Y., in Portage strata^ VIII f. Goniatites chemungensis. Vanuxem, Geology
RMRD7NCY–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ind.1881. Hall,28th Rt., 1876 ; Fenestella ambigua, Hall, 28th Rt., 1879). CoUett's Indiana Report of 1881, page 248, plate 10, figs.p? to 21. In well-preserved specimens there are rows of minute pits between the striae.—Niagara, Vb. lionchocephalus chippewaensis (Conccephalus chippe-. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations ma
RMPFYH3E–. Fresh-water biology. Freshwater biology. Fig. 0.1 MM. ' 1131. Alona intermedia. 166(151) With oblique Striae Alonella karua Turn to the key at the number indicated where the species named is discussed. 232 167 (137) Rostrum broad, semicircular Graptoleberis Sars 1863. Sole species Graptoleberis iestudinaria (Fischer) 1848. Posterior margin with 2 strong teeth at infero-posteal angle; valves and head with conspicuous reticulation. Head large; fornix very broad, forming a semicircular rostrum, covering anteimules and extend- ing down as far as ventral margin of valves. Post-abdomen bent at the
RMRDDY7T–. The anatomy of the common squid, Loligo pealii, Lesueur. Squids; Mollusks. 31 cutting edge of the jaw. This edge is drawn up into a strong median tooth which is flanked by a pair of small notches. The pharyngeal muscles are attach- ed to the adjacent surfaces of the lamellae of each jaw and fill the narrow space between them. The jaws grow constantly by additions to their margin's and to their unexposed surfaces. They are marked by two sets of fine striae, the lines of growth, one set concentric with the point of the jaw and one set radiating from it. The jaws are brown- ish-black on the cut
RMPFXF7M–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 857 Rens. lected figs. 16, 17, dorsal and ventral views of a characteristic specimen somewhat larger than common; 18, unusual, broad, ventral valve; 19, dorsal cast, with muscular scars, dental cav- ities, etc., 20, ventral cast with scars, and hinge plate impres- sion. Characteristic radiating striae uf Rensselmria not ob- served. If a different genus. Hall proposed the name Rens- selandia. Found in an Upper Helderherg limestone at Water- loo, Iowa.—In Penns
RMRD7NGF–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Ind.1881. Hall,28th Rt., 1876 ; Fenestella ambigua, Hall, 28th Rt., 1879). CoUett's Indiana Report of 1881, page 248, plate 10, figs.p? to 21. In well-preserved specimens there are rows of minute pits between the striae.—Niagara, Vb. lionchocephalus chippewaensis (Conccephalus chippe-. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations ma
![. Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 489 26 (27) Lateral dots much accentuated Spilophora Bastian. The striae are resolvable into rows of dots which are much accentuated on the lateral fields. Genus of a score or more known species, aquatic, mostly marine. Representative species. Spilophora canadensis Cobb 1914.. &. ; 15. â ^: 4.V- 88.4 â "SY.i â Lateral wings {3) are very prominent, and pos- teriorly are somewhat scalariform. The females have symmetrically reflexed ovaries. Habitat: Fresh-water ponds. Cape Breton Is- land, Dominion of Canada. Fig. 786. Spi Stock Photo](https://c8.alamy.com/comp/PFW0DA/fresh-water-biology-freshwater-biology-free-living-nematodes-489-26-27-lateral-dots-much-accentuated-spilophora-bastian-the-striae-are-resolvable-into-rows-of-dots-which-are-much-accentuated-on-the-lateral-fields-genus-of-a-score-or-more-known-species-aquatic-mostly-marine-representative-species-spilophora-canadensis-cobb-1914-amp-15-4v-884-quotsyi-lateral-wings-3-are-very-prominent-and-pos-teriorly-are-somewhat-scalariform-the-females-have-symmetrically-reflexed-ovaries-habitat-fresh-water-ponds-cape-breton-is-land-dominion-of-canada-fig-786-spi-PFW0DA.jpg ". Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 489 26 (27) Lateral dots much accentuated Spilophora Bastian. The striae are resolvable into rows of dots which are much accentuated on the lateral fields. Genus of a score or more known species, aquatic, mostly marine. Representative species. Spilophora canadensis Cobb 1914.. &. ; 15. â ^: 4.V- 88.4 â "SY.i â Lateral wings {3) are very prominent, and pos- teriorly are somewhat scalariform. The females have symmetrically reflexed ovaries. Habitat: Fresh-water ponds. Cape Breton Is- land, Dominion of Canada. Fig. 786. Spi Stock Photo")
RMPFW0DA–. Fresh-water biology. Freshwater biology. FREE-LIVING NEMATODES 489 26 (27) Lateral dots much accentuated Spilophora Bastian. The striae are resolvable into rows of dots which are much accentuated on the lateral fields. Genus of a score or more known species, aquatic, mostly marine. Representative species. Spilophora canadensis Cobb 1914.. &. ; 15. â ^: 4.V- 88.4 â "SY.i â Lateral wings {3) are very prominent, and pos- teriorly are somewhat scalariform. The females have symmetrically reflexed ovaries. Habitat: Fresh-water ponds. Cape Breton Is- land, Dominion of Canada. Fig. 786. Spi
RMRE9NPD–. Contributions from the Botanical Laboratory, vol. 8. Botany; Botany. Fig. 3 Cellulose wall of dead elder pith cells showing end-to-end orientation of linear micelles in parallel striae, surface view. the living cells of Allium. Some of the results were obtained in cooperation with Mr. Spierer in his laboratory in Geneva. I am greatly indebted to him for his technical assistance and continued interest in my work which involves the use of his lens. Since writing the first draft of the manuscript of this article I have learned from Mr. Spierer that he too has continued our first investigations
RMPFXJKM–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Indmx narrow; lamelL'B 120, alternating in length, the longer ones becoming bundles as they near the hottom,— Corniferous lime- stone at Falls of Ohio.— VIII a, Cyathophayllum concentricum. (Hall, 35th An. Kt.N. Y. Mils. 1882, page 146.) Collett's In- diana Et. 1882, page 316, plate 21, fig. 1.— fossette extends from near center to front margin; lamellae 100, of nearly uniform size at margin, alternating below; when skinned the specimen shows internal striae
RMRDY5KJ–. The anatomy of the domestic animals . Veterinary anatomy. THE HOOF 891. ndge formed by the junction of the frog with the bar and sole. This surface presents fine striae and openings for the papillae of the corium. The external or grotand surface presents a central sulcus (Sulcus cunei), which is bounded by two ridges or crura (Crura cunei). The medial and lat- eral surfaces (Facies medialis et lat- eralis) are united at the upper part with the bars and sole, but are free below and form the central wall of the deep collateral sulci (Sulci para- cuneati), which are bounded out- wardly by the b
RMPFXK2X–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 475 NUCUL. Nuculites {Orthonota) carinata, Hall. Dawson's Acad. ^v-w ..r-^. 207 Qeol. 1868, p. 602, fig. 207; sharp keel ex- tending from the beak obliquely to back pavv.-'«^=s:=3=;^^**— base; space in front of the keel marked by distinct, raised lamellose striae, and intermediate finer ones; space between this and hinge line smooth and slightly de- pressed ; hinge line forward of beak has six or seven crenula- tions; strong clavicle curves gently backward.—
![. Report upon the palaeontology of the province of Ontario [microform]. Paleontology; Paléontologie. HK) of a fenohtrulo, Huparntod by obscure mid dclioaU; undulntint; striae. Rovorw npparontl^ HIUOOlll. I huvc little doubt as to the identity of our .spcciiiit^iiH witl> ihoso dettcribed by I'rout. tb'tuyh tluT//i'>ni liiullii (Nieholson), (liDlnijinil Mtiijir.iiir, April, 1^74. i'olyznary small, {'orniin^ a flattened expansion ; branches radiating; from the base, and inerca.sin^ by bifurcation at intervals of about two lines. HranehcH nairow, about eight in the space of a ijuarter of an Stock Photo](https://c8.alamy.com/comp/RJ4GXM/report-upon-the-palaeontology-of-the-province-of-ontario-microform-paleontology-palontologie-hk-of-a-fenohtrulo-huparntod-by-obscure-mid-dclioau-undulntint-striae-rovorw-npparontl-hiuoolll-i-huvc-little-doubt-as-to-the-identity-of-our-spcciiiitiih-witlgt-ihoso-dettcribed-by-irout-tbtuyh-tlutigtni-liiullii-nieholson-lidlnijinil-mtiijiriiir-april-174-iolyznary-small-orniin-a-flattened-expansion-branches-radiating-from-the-base-and-inercasin-by-bifurcation-at-intervals-of-about-two-lines-hranehch-nairow-about-eight-in-the-space-of-a-ijuarter-of-an-RJ4GXM.jpg ". Report upon the palaeontology of the province of Ontario [microform]. Paleontology; Paléontologie. HK) of a fenohtrulo, Huparntod by obscure mid dclioaU; undulntint; striae. Rovorw npparontl^ HIUOOlll. I huvc little doubt as to the identity of our .spcciiiit^iiH witl> ihoso dettcribed by I'rout. tb'tuyh tluT//i'>ni liiullii (Nieholson), (liDlnijinil Mtiijir.iiir, April, 1^74. i'olyznary small, {'orniin^ a flattened expansion ; branches radiating; from the base, and inerca.sin^ by bifurcation at intervals of about two lines. HranehcH nairow, about eight in the space of a ijuarter of an Stock Photo")
RMRJ4GXM–. Report upon the palaeontology of the province of Ontario [microform]. Paleontology; Paléontologie. HK) of a fenohtrulo, Huparntod by obscure mid dclioaU; undulntint; striae. Rovorw npparontl^ HIUOOlll. I huvc little doubt as to the identity of our .spcciiiit^iiH witl> ihoso dettcribed by I'rout. tb'tuyh tluT//i'>ni liiullii (Nieholson), (liDlnijinil Mtiijir.iiir, April, 1^74. i'olyznary small, {'orniin^ a flattened expansion ; branches radiating; from the base, and inerca.sin^ by bifurcation at intervals of about two lines. HranehcH nairow, about eight in the space of a ijuarter of an
RMPFX8YB–. A manual for the study of insects. Insects. The Hermit Flower-beetle, Osrnoderma ereniicola (Os-mo- der'ma er-e-mic^o-la).—This is one of the larger of our Flower-beetles (Fig. 684). It is of a deep mahogany-brown color, nearly smooth, and highly polished. It is sup- posed that the larva lives on decaying wood in forest-trees. The Rough Flower-beetle, Osmoderma scabra (O. sca^bra), is closely allied to the preceding. It is not quite as large, meas- uring; about one inch in length. It is purplish black, and the wing-covers are roughened with irregular, coarsely-punc- tured striae. It is noctu
![. The colossal cephalopods of the North Atlantic [microform]. Cephalopoda; Squids; Octopuses; Céphalopodes; Calmars; Poulpe. 81 COLOSSAL CEPHALOPODS. posterior end, the length from tlie point of the beak to the poste- rior edge being 3'4 inches. The texture is firmer and the lamina are relatively thiclier than in A. monachua. Tlio rostrum and most of the frontal regions arc black and polished, gradually be- coming orange-brown and translucent toward the posterior border, and marked with faint striae radiating from the tip of the beak, and Fig. 20.. tm Lowerjawof Archlteuthlaprinccps. No. 10. N Stock Photo](https://c8.alamy.com/comp/REP0P1/the-colossal-cephalopods-of-the-north-atlantic-microform-cephalopoda-squids-octopuses-cphalopodes-calmars-poulpe-81-colossal-cephalopods-posterior-end-the-length-from-tlie-point-of-the-beak-to-the-poste-rior-edge-being-34-inches-the-texture-is-firmer-and-the-lamina-are-relatively-thiclier-than-in-a-monachua-tlio-rostrum-and-most-of-the-frontal-regions-arc-black-and-polished-gradually-be-coming-orange-brown-and-translucent-toward-the-posterior-border-and-marked-with-faint-striae-radiating-from-the-tip-of-the-beak-and-fig-20-tm-lowerjawof-archlteuthlaprinccps-no-10-n-REP0P1.jpg ". The colossal cephalopods of the North Atlantic [microform]. Cephalopoda; Squids; Octopuses; Céphalopodes; Calmars; Poulpe. 81 COLOSSAL CEPHALOPODS. posterior end, the length from tlie point of the beak to the poste- rior edge being 3'4 inches. The texture is firmer and the lamina are relatively thiclier than in A. monachua. Tlio rostrum and most of the frontal regions arc black and polished, gradually be- coming orange-brown and translucent toward the posterior border, and marked with faint striae radiating from the tip of the beak, and Fig. 20.. tm Lowerjawof Archlteuthlaprinccps. No. 10. N Stock Photo")
RMREP0P1–. The colossal cephalopods of the North Atlantic [microform]. Cephalopoda; Squids; Octopuses; Céphalopodes; Calmars; Poulpe. 81 COLOSSAL CEPHALOPODS. posterior end, the length from tlie point of the beak to the poste- rior edge being 3'4 inches. The texture is firmer and the lamina are relatively thiclier than in A. monachua. Tlio rostrum and most of the frontal regions arc black and polished, gradually be- coming orange-brown and translucent toward the posterior border, and marked with faint striae radiating from the tip of the beak, and Fig. 20.. tm Lowerjawof Archlteuthlaprinccps. No. 10. N
RMPFXJRF–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. P(.9 tm.A.G. 1855. 3e 5a I. 'Hi' jim ditto, hinge; 5 e, ditto, front; fflim ^ '^' ditto, striae on the surface. Oincmna ti group. Ill J.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lesley, J. P. (J. Peter), 1819-1903; Pennsylvania. Board of Commissioners for the Second Geological Su
![. Fungi; their nature, influence, and uses;. Fungi. Fig. 10.—a. Threads of Trichia. 6. Portion furtber magnified, with spores, c. Por- tion of spinulose thread. on these threads has been whether the spiral markings are external or internal, whether caused by twisting of the thread or by the presence of an external or internal fibre. The spiral appearance has never been called in question, only the structure from whence it arises, and this, like the striae of diatoms, is very much an open question. Mr. Currey held that the spiral * Wigand, '' Morpliologie dcs Genres Trichia et Arcyria," in Stock Photo](https://c8.alamy.com/comp/RE1GP7/fungi-their-nature-influence-and-uses-fungi-fig-10a-threads-of-trichia-6-portion-furtber-magnified-with-spores-c-por-tion-of-spinulose-thread-on-these-threads-has-been-whether-the-spiral-markings-are-external-or-internal-whether-caused-by-twisting-of-the-thread-or-by-the-presence-of-an-external-or-internal-fibre-the-spiral-appearance-has-never-been-called-in-question-only-the-structure-from-whence-it-arises-and-this-like-the-striae-of-diatoms-is-very-much-an-open-question-mr-currey-held-that-the-spiral-wigand-morpliologie-dcs-genres-trichia-et-arcyriaquot-in-RE1GP7.jpg ". Fungi; their nature, influence, and uses;. Fungi. Fig. 10.—a. Threads of Trichia. 6. Portion furtber magnified, with spores, c. Por- tion of spinulose thread. on these threads has been whether the spiral markings are external or internal, whether caused by twisting of the thread or by the presence of an external or internal fibre. The spiral appearance has never been called in question, only the structure from whence it arises, and this, like the striae of diatoms, is very much an open question. Mr. Currey held that the spiral * Wigand, '' Morpliologie dcs Genres Trichia et Arcyria," in Stock Photo")
RMRE1GP7–. Fungi; their nature, influence, and uses;. Fungi. Fig. 10.—a. Threads of Trichia. 6. Portion furtber magnified, with spores, c. Por- tion of spinulose thread. on these threads has been whether the spiral markings are external or internal, whether caused by twisting of the thread or by the presence of an external or internal fibre. The spiral appearance has never been called in question, only the structure from whence it arises, and this, like the striae of diatoms, is very much an open question. Mr. Currey held that the spiral * Wigand, '' Morpliologie dcs Genres Trichia et Arcyria," in
RMPFXXRN–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 705 Pleu. Acad. Nat. Sci. Phila. Vol. 8, Trenton and Hudson river for- mations. Hall., Pal. N. Y. Vol. 1,1847, page 305, plate 83,lig. 4 a^ small, showing back of spire and expansion of last whorl; J, enlarged surface to show alternating larger and smaller carinas (keels) crossed by the oblique fine striae; c, larger specimen; ^, another with aperture entire on the outer mar- gin ; g, base. Resembles P. Ucarinata of the Trenton forma- tion^hMt differs essenti
RMRDXNXF–. The anatomy of the domestic animals . Veterinary anatomy. 782 NERVOUS SYSTEM OF THE HORSE base blends in front with the junction of the striae medullares of the thalamus. Immediately under the posterior part of the stalk is a short transverse band of white matter, the posterior commissure of the cerebrimi (Commissura aboralis cerebri). The pineal body is enclosed in a fibrous capsule from which numerous trabeculae pass inward, dividing the organ into spaces occupied by round epitheUal cells of the same origin as the epen- dyma of the ventricle. The mammillary body (Corpus mammillare) is a wh
RMPFXXM7–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. v»r.tt Hall 6^'... or Western District, of New York, 1843, page 172, fig. 68. 1, a perfect speci- men; showing equal valves; hind wing; radiat- ing fine striae; prominent growth lines; large promi- nent beak. Perfect casts were also found at the place (Clarence Hollow, N. Y.). It clo5!ely resembles a Pterinea (Megambonia) of the Oriskany sandstone.— Corniferous (Upper Hel- derherg) limestone forma- tion.— VIII a. Megambonia jamesi, Meek. See Appendix, Megambo
RMRDA363–. Fresh-water biology. Freshwater biology. THE WATER-MITES (HYDRACARINA) 853 or laterally, and in the males of certain species of Arrhenurus pro- longed posteriorly into a curious handle-like appendage. The form is more definite in the higher forms than in those which seem most primitive. The skin in some forms is soft and the surface smooth, but more usually it is marked by fine striae like the lines on the palm of the hand, and in the lower forms it is often granulated or papillated. Other species possess chitinous plates, which may be few and small or larger and more numerous, and may even
RMPFXGE2–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. NXVoljy Jb. ISO 180, plate 26, figs. 9 to 15. Characterized by small ribs. The dorsal valves, interior surface alone known, are deeply con- caved. Inner surface strongly papillose-striate and shows con- centric striae. Species somewhat like P, dumosa^ of the Ham- ilton rocks. Dorsal valve like P. striatula. but can be distin- guished by its numerous minute pustules inside. Many places in New York in Chemung formation,—In Pennsylvania col- lected by Carll &
RMRD958W–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 233, plate 78 B^ fig. 2, a portion of Hall's complete figure, show- ing only the inhabited chamber, and the three narrow chambers behind it, eight others to the smaller end being cut off; also the open end of the large chamber cut ofi*. The scratches (striae) on one part of the surface are bent to a middle line, not because this is their natural mode of appearance, but the animal thus repaired some violent fracture of its shell, which was thereby thickened an
RMPFXJ07–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. Orthoceras subcancellatum, Hall, in Collett's Indiana Vb^nmnMimK r -I^^P^^^ ^^ ISSl, page 323, plate ?>3^ fig. 5. (0. cancellatum. Hall, Pal. N. Y. Vol. 2, page 292; not 0. cancellatum .of Eich- wald, 1842.) Surface ornamented with angular ridges lengthwise, between w^hich run finer striae, crossed by finer equal % striae, which gives the cancellated ap- pearance. Rare at Waldron, Ind., and then only as inside casts preserving only the long ridges and line
RMRDJ2BN–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. lOS FAMILY IT. CAEABin.+;. ee. Sides of thorax not flattened; prosternum without setae; piceous. shining. 166. chalcea. dd. Prostenmm of male smooth as in the females and without setse; sides of thorax not flattened. ^ /'. Elytral striae fine, the intervals flat; thorax distinctly emarginate at apex. 167. sub^nea. ff. Elytral strife deep, the intervals convex: thorax nearly trimcate at apex. g. Foim oblnng;
RMPFYHB5–. Fresh-water biology. Freshwater biology. 698 FRESH-WATER BIOLOGY 39 (25) Cervical sinus present. No crest 40 40 (45) Valves transversely striated. Post-abdomen broad, with indenta- tion in which anus opens. Simocephalus Schoedler 1858 . 41 Body large and heavy; shell thick. Head and rostrum small. Valves large, somewhat quadrate, with rounded angles and sometimes a posterior spine; marked with oblique striae, anastomosing irregularly and with cross-connections. Two abdominal processes developed, placed far apart. Post-abdomen large, broad, truncate, posterior end emarginate and bear- ing the
RMRDJ1P7–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE STAG BEETLES. 907 bles with a large median tooth which points obliquely inward and upward. Elytra deeply striate, both striae and intervals finely and rather closely punctured. Length 15-26 mm. Throughout the State; frequent. April 27-December 8. Hi- bernates beneath old, partly burned logs. Occurs most commonly in June and July about the roots of oak, linn and maple trees and stumps, in the decaying woo
RMPFXJ0B–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 559 Orthoc.. Orthoceras subcancellatum, Hall, in Collett's Indiana Vb^nmnMimK r -I^^P^^^ ^^ ISSl, page 323, plate ?>3^ fig. 5. (0. cancellatum. Hall, Pal. N. Y. Vol. 2, page 292; not 0. cancellatum .of Eich- wald, 1842.) Surface ornamented with angular ridges lengthwise, between w^hich run finer striae, crossed by finer equal % striae, which gives the cancellated ap- pearance. Rare at Waldron, Ind., and then only as inside casts preserving only the long ri
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. Ml i m- ] 604 THE UPPER SILURIAN. convex, scarcely gibbous; umbonlal slope regularly convex, below which is a slight depression reaching to tiie postero-basal margin; posterior end rounded, the longer part of the curve on the basal side. Anterior end short and narrow, somewhat abruptly rounded. Surface marked by regularly radiating rounded striae with fain Stock Photo](https://c8.alamy.com/comp/RJ5KD7/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-ml-i-m-604-the-upper-silurian-convex-scarcely-gibbous-umbonlal-slope-regularly-convex-below-which-is-a-slight-depression-reaching-to-tiie-postero-basal-margin-posterior-end-rounded-the-longer-part-of-the-curve-on-the-basal-side-anterior-end-short-and-narrow-somewhat-abruptly-rounded-surface-marked-by-regularly-radiating-rounded-striae-with-fain-RJ5KD7.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. Ml i m- ] 604 THE UPPER SILURIAN. convex, scarcely gibbous; umbonlal slope regularly convex, below which is a slight depression reaching to tiie postero-basal margin; posterior end rounded, the longer part of the curve on the basal side. Anterior end short and narrow, somewhat abruptly rounded. Surface marked by regularly radiating rounded striae with fain Stock Photo")
RMRJ5KD7–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. Ml i m- ] 604 THE UPPER SILURIAN. convex, scarcely gibbous; umbonlal slope regularly convex, below which is a slight depression reaching to tiie postero-basal margin; posterior end rounded, the longer part of the curve on the basal side. Anterior end short and narrow, somewhat abruptly rounded. Surface marked by regularly radiating rounded striae with fain
RMPFXGGE–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. MURC. 428 preserved, showing the characteristic generic arched or undu- lating strias. Specimen found near Newark, Wayne Co., N. Y., but not yet in Pennsylvania Salina rochs^ Vc. Murchisonia ? confusa. Whitfield. Ila, See Appendix, MurcUsonia conula. See Pleurotomaria conula. XI. Murchisonia desiderata, Hall. 15th Annual Report, N Y., Wl a :fj?. 1862,page 50,plate 4,fig. 12. — Upper Heldevlerg for- mation^ VIII a. Concen- tric striae on the surface ^r^m^^ ..
RMRD8MDG–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 10th Regents Rt. 1857. Chemung,) Hall, Pal.N. Y. Vol. IV, 1867, page 170, plate 24, figs. 1 to 9. It occurs in the same beds with P. loydii and P. hirsuta^ but is easily distinguished from them by its greater gibbosity and fewer spines; and its casts, by extremely fine papillas and their extension in hairlike striae. In general characters it resembles P. suhalataoH the Hamilton formation^ in Illinois. Found in the ChemunghedsdX Phillips- burg, Alleghany Co.,
RMPFXHY5–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 75, plate 7, fig. 4. Nearly all specimens are a little flattened by rock pressure. Rings in two specimens 8 and 9 in the same length. Siphuncle of one an inch thick is a little over three-twentieths of an inch wide. Ring ridges are direct., thus differing from the Niagara species; as also in having striae lengthwise. It tapers less than the ringed Hamilton species. —Schoharie grit.. East N. Y. VII h. — In Pennsylvania, found at Dingman's Falls, Pike Co. Spec.
RMRDTRAD–. A monograph of the Mycetozoa, being a descriptive catalogue of the species in the herbarium of the British Museum. Illustrated with seventy-eight plates and fifty-one woodcuts. Myxomycetes. Fig. 20. Lime-crystals heaped together, at first concealing the confluent hollow sporangiar. (13) Spumaria. Fig. 21.—Spumaria alia DC. a. -Sthalium. Natural size. J. Capillitium and fragment of sporangium-wall, with crystals of calcium carbonate and two spores. Magnified 200 times.. Fig. 21. Lime-crystals lenticular, marked with radiating striae, scattered over the sporangium-wall. (14) Lepidoderma. Fig.
![. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE LEAF BEETLES. 1143 KEY TO IXDlA^s'A SPECKS 01- FIDLi. (/. I'iiecus ur nearly black; iiuuetures of elytral striie coarse and deeij; intervals flat, punctures not densu. 2115. loxgipes. 0(7. Reddish to pale brown; punctures of elytral striae not very coarse; In- tervals flat, densely punctured. 2116. viticida. 2115 (i">724i. FiDiA LOXGIPES Melsh., l'i;<r. Phil. Acad. Nat. Sci., Ill, 1S4T. 169. E Stock Photo](https://c8.alamy.com/comp/PG3H36/an-illustrated-descriptive-catalogue-of-the-coleoptera-or-beetles-exclusive-of-the-rhynchophora-known-to-occur-in-indiana-with-bibliography-and-descriptions-of-new-species-beetles-the-leaf-beetles-1143-key-to-ixdlasa-specks-01-fidli-iiiecus-ur-nearly-black-iiuuetures-of-elytral-striie-coarse-and-deeij-intervals-flat-punctures-not-densu-2115-loxgipes-07-reddish-to-pale-brown-punctures-of-elytral-striae-not-very-coarse-in-tervals-flat-densely-punctured-2116-viticida-2115-iquotgt724i-fidia-loxgipes-melsh-liltr-phil-acad-nat-sci-ill-1s4t-169-e-PG3H36.jpg ". An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE LEAF BEETLES. 1143 KEY TO IXDlA^s'A SPECKS 01- FIDLi. (/. I'iiecus ur nearly black; iiuuetures of elytral striie coarse and deeij; intervals flat, punctures not densu. 2115. loxgipes. 0(7. Reddish to pale brown; punctures of elytral striae not very coarse; In- tervals flat, densely punctured. 2116. viticida. 2115 (i">724i. FiDiA LOXGIPES Melsh., l'i;<r. Phil. Acad. Nat. Sci., Ill, 1S4T. 169. E Stock Photo")
RMPG3H36–. An illustrated descriptive catalogue of the coleoptera or beetles (exclusive of the Rhynchophora) known to occur in Indiana : with bibliography and descriptions of new species . Beetles. THE LEAF BEETLES. 1143 KEY TO IXDlA^s'A SPECKS 01- FIDLi. (/. I'iiecus ur nearly black; iiuuetures of elytral striie coarse and deeij; intervals flat, punctures not densu. 2115. loxgipes. 0(7. Reddish to pale brown; punctures of elytral striae not very coarse; In- tervals flat, densely punctured. 2116. viticida. 2115 (i">724i. FiDiA LOXGIPES Melsh., l'i;<r. Phil. Acad. Nat. Sci., Ill, 1S4T. 169. E
RMRDTR6E–. A monograph of the Mycetozoa, being a descriptive catalogue of the species in the herbarium of the British Museum. Illustrated with seventy-eight plates and fifty-one woodcuts. Myxomycetes. Fig. 20. Lime-crystals heaped together, at first concealing the confluent hollow sporangiar. (13) Spumaria. Fig. 21.—Spumaria alia DC. a. -Sthalium. Natural size. J. Capillitium and fragment of sporangium-wall, with crystals of calcium carbonate and two spores. Magnified 200 times.. Fig. 21. Lime-crystals lenticular, marked with radiating striae, scattered over the sporangium-wall. (14) Lepidoderma. Fig.
RMPFXXPC–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. p, cLurhajnCfss Wit^ ada, 111, i, 1884, page 23, plate 3, fig. 12, side view of a speci- men from Durham, Canada West; 12 ^, another showing mouth; crowded transverse striae; shell extremely thickened at the periphery of the last volute, so as to make an exactly circular mouth; a curious feature seen also in Pterocheilus primus^ Moore, from English Lias, Differs from P. hispiralis^ Hall, in more obliquely flattened spire, etc.— Guelph formation. Vb Pleurotom
![. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. (Hall,35th An. Rt. Mus. 1882.) Oollett's Indian Rt., 1882, page 303, plate 27; figs. 7,8.— Falls of Ohio, Corniferous limestone.— Villa. The genus is Lonsdale's. Hall's description of the spe- cies on page 458 of the 35th An. Rt. is as follows: " Oor- allum sub-cylindrical, simple or compound, increasing by lateral gemmation, fre- quently in contact for their entire length; exterior with very regular annulations and concentric striae; longitudinal striae Stock Photo](https://c8.alamy.com/comp/RD95JX/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-hall35th-an-rt-mus-1882-oolletts-indian-rt-1882-page-303-plate-27-figs-78-falls-of-ohio-corniferous-limestone-villa-the-genus-is-lonsdales-halls-description-of-the-spe-cies-on-page-458-of-the-35th-an-rt-is-as-follows-quot-oor-allum-sub-cylindrical-simple-or-compound-increasing-by-lateral-gemmation-fre-quently-in-contact-for-their-entire-length-exterior-with-very-regular-annulations-and-concentric-striae-longitudinal-striae-RD95JX.jpg ". A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. (Hall,35th An. Rt. Mus. 1882.) Oollett's Indian Rt., 1882, page 303, plate 27; figs. 7,8.— Falls of Ohio, Corniferous limestone.— Villa. The genus is Lonsdale's. Hall's description of the spe- cies on page 458 of the 35th An. Rt. is as follows: " Oor- allum sub-cylindrical, simple or compound, increasing by lateral gemmation, fre- quently in contact for their entire length; exterior with very regular annulations and concentric striae; longitudinal striae Stock Photo")
RMRD95JX–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. (Hall,35th An. Rt. Mus. 1882.) Oollett's Indian Rt., 1882, page 303, plate 27; figs. 7,8.— Falls of Ohio, Corniferous limestone.— Villa. The genus is Lonsdale's. Hall's description of the spe- cies on page 458 of the 35th An. Rt. is as follows: " Oor- allum sub-cylindrical, simple or compound, increasing by lateral gemmation, fre- quently in contact for their entire length; exterior with very regular annulations and concentric striae; longitudinal striae
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