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443 results for “Cephalopod”
Figure 2 in Spatiotemporal patterns in marine fish and cephalopods communities across scales: using an autoregressive spatiotemporal clustering model. A study of fish and cephalopods of the Eastern English Channel
Figure 2. – Spatial correlation matrix at a 522 km2 scale displaying correlation from strongly negative (dark blue) to strongly positive (dark red).
Figure 11 in Spatiotemporal patterns in marine fish and cephalopods communities across scales: using an autoregressive spatiotemporal clustering model. A study of fish and cephalopods of the Eastern English Channel
Figure 11. – Scophthalmus rhombus from low (blue) to high (red) median densities of numbers/ km2 in log scale for 522 km2 for the Eastern English Channel.
Figure S5 in Spatiotemporal patterns in marine fish and cephalopods communities across scales: using an autoregressive spatiotemporal clustering model. A study of fish and cephalopods of the Eastern English Channel
Figure S5. – Spatial-temporal hierarchical clustering at a 782 km2 (A) and 1043 km2 (B) scale. The rectangle outlines the communities that where find statistically significant by ASTEC given the approximately unbiased p-values expressed as proportion (red).
Fig. 5 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea
Fig. 5 Camera lucida drawings of Triassic orthoceratoid genera (not to scale) in comparison with Michelinoceras. Phattalungoceras is not shown here, as the only specimen is too poorly preserved to confidently reconstruct its internal structures, although it appears to resemble Pseudotemperoceras. A Michelinoceras michelini, after Barrande (1870; pl. 381; fig. 14); B Trematoceras elegans, after Schindewolf (1933; fig. 5); C Paratrematoceras shevyrevi, after Schastlivceva (1988 pl. 1, fig. 3); D Pseudotemperoceras nyalamense, after Chen (1981; text-fig. 2); E Pseudotemperoceras pulchrum, after Schastlivceva (1988; pl. 1, fig. 5c)
Fig. 6 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea
Fig. 6 Comparison of embryonic shells of selected orthoceratoids. A Trematoceras cf. politum (= T. elegans), Late Triassic, Carnian, after Schindewolf (1933; fig. 5). B Michelinoceras michelini, late Silurian, Ludlow, after Ristedt (1968; fig. 3.1b); C Pseudorthoceras knoxense, Carboniferous, Serpukhovian, after Kröger & Mapes (Kröger & Mapes, 2004; fig. 5.9)
Fig. 7 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea
Fig. 7 Simplified time-scaled phylogeny demonstrating possible relationships of the Trematoceratidae to other orthoceratoids and coleoids. Note that Orthoceras and Michelinoceras are more closely related to coleoids than they are to trematoceratids under this concept. Several groups are omitted here for clarity (e.g., Nautilida, Ammonoida). The questionable Zhuravlevia is here excluded
Fig. 52. Discoscaphites jerseyensis, n in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 52. Discoscaphites jerseyensis, n.sp., macroconchs, Pinna Layer, top of the Tinton Formation, Manasquan River Basin, Monmouth County, New Jersey. A–D. AMNH 50393, holotype. A. Right lateral; B. apertural; C. ventral; D. left lateral. E–H. AMNH 50774, paratype. E. Right lateral; F. apertural; G. ventral; H. left lateral. All figures X1.
Fig. 46 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 46. Size frequency histogram of a sample of Discoscaphites iris (Conrad, 1858) from the upper part of the Tinton Formation, mostly the Pinna Layer, Manasquan River Basin, Monmouth County, New Jersey.
Fig. 51 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 51. Discoscaphites gulosus (Morton, 1834), macroconch, MAPS A2025c1, Pinna Layer, top of the Tinton Formation, Manasquan River Basin, Monmouth County, New Jersey. A. Lateral view of part of the shaft; B. ventral view. Both figures X1.
Fig. 50 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 50. Discoscaphites minardi Landman et al., 2004a, macroconchs, or indeterminate (as indicated), Pinna Layer, and underlying part of Tinton Formation (as indicated), Manasquan River Basin, Monmouth County, New Jersey. A–C. AMNH 50760, underlying part of the Tinton Formation. A. Right lateral; B. ventral; C. left lateral. D,E. AMNH 50759. D. Right lateral; E. ventral. F,G. AMNH 50758, dimorph indeterminate, but probably a microconch. F. Ventral; G. left lateral. H,I. AMNH 50761.
Fig. 44 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 44. Discoscaphites iris (Conrad, 1858). A–Q. Pinna Layer, Tinton Formation, and reworked material at the base of the Hornerstown Formation (as indicated), Manasquan River Basin, Monmouth County, New Jersey. A,B. MAPS A2060b34, a microconch. A. Ventral; B. left lateral. C,D. MAPS A2060b33, a microconch. C. Ventral; D. left lateral. E. MAPS A2060b1, part of a cluster of juveniles, with the bottom side down. F–I. AMNH 50711, a microconch. F. Right lateral; G. apertural; H. ventral; I. left
Fig. 38 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 38. Top. Size histogram of a sample of Eubaculites latecarinatus (Brunnschweiler, 1966), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. Most of the specimens are fragments of juvenile body chambers. Bottom. Scatter plot of whorl width versus height in the same sample of E. latecarinatus. Measurements are at the adoral ends of the specimens.
Fig. 37 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 37. Eubaculites latecarinatus (Brunnschweiler, 1966), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–E. AMNH 51877. A. Right lateral; B. dorsal; C. ventral; D. left lateral; E. whorl section at adoral end. F–I. AMNH 51876. F. Right lateral; G. dorsal; H. ventral; I. left lateral. J–M. AMNH 51862. J. Right lateral; K. dorsal; L. ventral; M. left lateral. N–Q. AMNH 51875. N. Right lateral; O. dorsal; P. ventral; Q. left lateral. All figures X1.
Fig. 43 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 43. Discoscaphites iris (Conrad, 1858), macroconchs. A–E, G–S. Pinna Layer and the underlying part of the Tinton Formation (as indicated), Manasquan River Basin, Monmouth County, New Jersey. A– D. AMNH 50398, slightly crushed, underlying part of the Tinton Formation. A. Right lateral; B. apertural; C. ventral; D. left lateral. E. AMNH 50387, small specimen, partially sideritized, left lateral. G,H. AMNH 50756. G. Right lateral; H. ventral. I,J. AMNH 50389. I. Right lateral; J. ventral. K–M.
Fig. 36 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 36. Eubaculites latecarinatus (Brunnschweiler, 1966), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A,B. AMNH 50419. A. Ventral; B. right lateral. C– G. AMNH 50435. C. Right lateral; D. dorsal; E. ventral; F. left lateral; G. whorl section at adapical end. H–L. AMNH 51888. H. Right lateral; I. dorsal; J. ventral K. left lateral; L. whorl section at adoral end. M–P. AMNH 51874. M. Right lateral; N. dorsal; O. ventral; P. left lateral. Q–U. AMNH 51864. Q. Right lateral; R. dorsal; S. ventral; T. left lateral; U. whorl section at adapical end. V–Y. AMNH 51863. V. Right lateral; W. dorsal; X. ventral; Y. left lateral. All figures X1.
Fig. 35 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 35. Top. Size histogram of a sample of Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County. Nearly all of the specimens are fragments of juvenile body chambers with some exceptions, notably the two largest specimens (AMNH 50766 and MAPS A2058b1), which are presumably mature macroconchs. Bottom. Scatter plot of whorl width versus height in intercostal section in the same sample of E. carinatus. All measurements are at the adoral ends of the specimens. The Xs and Os represent measurements through the ontogeny of AMNH 50766 and MAPS A2058b1, respectively (the open circles indicate the septate portion of MAPS A2058b1; AMNH 50766 is completely septate.) The triangle represents another large body chamber (MAPS A2058b2), presumably a macroconch.
Fig. 34 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 34. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A. AMNH 50723, composite suture at WH 5 16.7 mm. B. AMNH 50778, suture at WH 5 22.2 mm. C. AMNH 50721, suture at WH 5 9.9 mm.
Fig. 33 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 33. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–D. AMNH 50721. A. Right lateral; B. dorsal; C. ventral; D. left lateral. E–H. AMNH 50767. E. Right lateral; F. dorsal; G. ventral; H. left lateral. I–M. AMNH 50768. I. Right lateral; J. dorsal; K. ventral; L. left lateral; M. whorl section at adapical end. N–Q. AMNH 50779. N. Right lateral; O. dorsal; P. ventral; Q. left lateral. All figures X1.
Fig. 31 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 31. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–D. AMNH 50781. A. Right lateral; B. dorsal; C. ventral; D. left lateral. E–H. AMNH 50418. E. Right lateral; F. dorsal; G. ventral; H. left lateral. I. AMNH 50737, mature microconch in matrix, with a possible apertural modification, right lateral. All figures X1.
Fig. 32 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 32. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–D. AMNH 50770. A. Right lateral; B. dorsal; C. ventral; D. left lateral. E–I. AMNH 50771. E. Right lateral; F. dorsal; G. ventral; H. left lateral; I. whorl section at adoral end. J–N. AMNH 50434. J. Right lateral; K. dorsal; L. ventral; M. left lateral; N. whorl section at adoral end with possible aptychus (arrow). O–S. AMNH 50765. O. Right lateral; P. dorsal; Q. ventral; R. left lateral; S. whorl section at adoral end. T–W. AMNH 50769. T. Right lateral; U. dorsal; V. ventral; W. left lateral. All figures X1.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
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The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
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