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Fig. 3 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 3. Ewing Creek (?) Member of the Lockatong Formation of the Granton Quarry and the Granton diabase sill, North Bergen, N.J. A, South side of existing hill capped by Granton sill, as it appeared in 1979. Sill is markedly discordant on the left; G0–G6 are cycle designations, and H shows the position of an in situ Hypuronector specimen (photo by P. Olsen). B, North side of same hill showing cycles G6–G8; H marks the probable horizon of the holotype near the base of cycle G7 based on lithological similarity (photo by David Stager, from Colbert, 1965). All of these units are still currently exposed.

Fig. 11 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 11. Forelimb of Hypuronector. A and B, YPM 56393, isolated forelimb drawings of part and counterpart slabs. C and D, AMNH 7759, forelimbs: (C) left manus, radius, and ulna and (D) right manus, radius and ulna. Identification of radius (r) and ulna (u) is not certain.

Fig. 14 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 14. Tentative cladogram of relationships within Drepanosauridae. Characters are: 1, caudal vertebrae with anteroposteriorly elongated, bladelike transverse processes through most of tail and with prezygapophyses of proximal caudals extending anteriorly well beyond centrum and postzygapophyses extending posteriodorsally from neural spine base; 2, postcervical vertebrae with zygophyseal facets generally very close to midline; 3, neural spines very long, especially on caudal vertebrae; 4, dorsal ribs firmly attached to centra; 5, hemal arches or chevrons fused to posterior part of anterior threequarters of caudal vertebrae and much greater in depth than height of the neural spines; 6, pectoral girdle with high and rodlike scapula; and 7, pelvic girdle with high, anteriorly directed blade of ilium. 8, Bifurcate or fenestrate chevrons; 9, distinctly enlarged and modified neural spines in shoulder region; 10, dorsal ribs fused to centra; 11, reduced manual and pedal phalangeal formula; 12, ''opposable'' digit I on pes; 13, giant ungual phalanx on manual digit II; 14, extremely deep tail. Note that Dolabrosaurus has no apparent unique derived characters. Dotted lines indicate less favored relationship indicated by character 10.

Fig. 13 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 13. Distal parts of the hind limb of Hypuronector. A, left hind limb; B, right hind limb.?I, is possible proximal phalanx of digit I.

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Fig. 24 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 2. Northeastern Monmouth County, New Jersey

Fig. 24. Sphenodiscus lobatus (Tuomey, 1856). A, B. MAPS A2002a8 (same specimen as in fig.

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Fig. 10 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 2. Northeastern Monmouth County, New Jersey

Fig. 10. Formational contact between the New Egypt and Hornerstown Formations at AMNH loc.

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Fig. 1 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 2. Northeastern Monmouth County, New Jersey

Fig. 1. Map of parts of New Jersey and Maryland showing localities mentioned in text.

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Fig. 3 in Additions to the Ammonite Fauna of the Upper Cretaceous Navesink Formation of New Jersey

Fig. 3. CampanianMaastrichtian macrofossil zonal successions in northwest Europe.

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Fig. 1 in Additions to the Ammonite Fauna of the Upper Cretaceous Navesink Formation of New Jersey

Fig. 1. Generalized stratigraphic succession

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Fig. 1 in Vulnerability of Northern Pine Snakes (Pituophis melanoleucus Daudin, 1803) during fall den ingress in New Jersey, USA

Fig. 1. Schematic of deployment of the Tracker device at the entrance of a hibernaculum.

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Fig. 11 in Primitive New Ants in Cretaceous Amber from Myanmar, New Jersey, and Canada (Hymenoptera: Formicidae)

Fig. 11. Partial worker of †Cananeuretus occidentalis? (TMP 91.149.3).

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Fig. 10 in Primitive New Ants in Cretaceous Amber from Myanmar, New Jersey, and Canada (Hymenoptera: Formicidae)

Fig. 10. Holotype worker of †Cananeuretus occidentalis, new genus and species (TMP 8.89.7).

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Fig. 7 in Primitive New Ants in Cretaceous Amber from Myanmar, New Jersey, and Canada (Hymenoptera: Formicidae)

Fig. 7. Facial view of holotype worker of †Haidomyrmex cerberus Dlussky (NHML In.20182).

Fig. 6 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 6. Holotype of AMNH 7759 (above) and drawing of holotype (below). Photograph by Chester Tarka.

Fig. 15 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 15. Reconstruction of Hypuronector. The cranium and number of cervical vertebrae

Fig. 10 in A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup)

Fig. 10. Shoulder girdle of Hypuronector