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Fig. 11 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. 11. Diagram of the contact between the New Egypt and Hornerstown Formations at AMNH loc. 3345, Parkers Creek, northeastern Monmouth County, New Jersey, showing the distribution of cephalopods and bivalves. Vertical scale = 35 cm; horizontal scale = 13 m. Not all of the fossils collected are shown nor do the symbols imply that the specimens are whole. The diagram is intended to provide an overview of the distribution of molluscan fossils, documenting that most of them occur at the formational contact.

Fig. 40. A–D, J–P 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. 40. A–D, J–P. Discoscaphites minardi Landman et al., 2004. A–D. MAPS A2059b2, macroconch, upper New Egypt Formation, 1.5–2 m below the base of the Hornerstown Formation, AMNH loc. 3347, northwest of Eatontown, Monmouth County, New Jersey. A, Left lateral; B, apertural; C, ventral; D, left lateral. J–M. AMNH 47307, macroconch, upper New Egypt Formation, 1.5–2 m below the base of the Hornerstown Formation, AMNH loc. 3346, northwest of Eatontown, Monmouth County, New Jersey. J. Right lateral; K, apertural; L, ventral; M, left lateral. N–P. AMNH 47305, microconch, same locality as J–M. N, Right lateral; O, ventral, P, left lateral. E–I, Q–S. Discoscaphites spp., same locality as J–P. E–G. AMNH 47301. E, Right lateral; F, ventral; G, left lateral. H, I. AMNH 47300. H, Right lateral; I, left lateral. Q–S. AMNH 47304. Q, Right lateral; R, ventral; S, left lateral. All specimens are X1.

Fig. 9. Dinoflagellates from USGS Paleobotan. loc. R6234 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. 9. Dinoflagellates from USGS Paleobotan. loc. R6234, lower part of the Hornerstown Formation, Parkers Creek, 0.3 km east of Rt. 35, northwest of Eatontown, northeastern Monmouth County,

Fig. 8. Dinoflagellates from USGS Paleobotan. loc. R6234 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. 8. Dinoflagellates from USGS Paleobotan. loc. R6234, upper part of the New Egypt Formation and lower part of the Hornerstown Formation, Parkers Creek, 0.3 km east of Rt. 35, northwest of

Fig. 7. Dinoflagellates from northeastern Monmouth County, New Jersey. A, B, H, I. USGS Paleobotan. loc. R6234E 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. 7. Dinoflagellates from northeastern Monmouth County, New Jersey. A, B, H, I. USGS Paleobotan. loc. R6234E, New Egypt Formation, approximately 1.5–2.0 m below the base of the Hornerstown Formation, Parkers Creek, 0.1 km east of Rt. 35, northwest of Eatontown. C, F, G. USGS Paleobotan.

Fig. 4 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. 4. Comparison of stratigraphic sections at localities in northeastern Monmouth County, New Jersey. Numbers correspond to those in the list of localities.

Fig. 6. Dinoflagellates from USGS Paleobotan. loc. R6234H 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. 6. Dinoflagellates from USGS Paleobotan. loc. R6234H, Tinton Formation, Hochhockson Brook, 0.2 km north of the intersection of Water Street and Tinton Avenue, northeastern Monmouth County, New Jersey. A–E. Isabelidinium cooksoniae (Alberti, 1959) Lentin & Williams, 1977 sensu lato.

Fig. 5 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. 5. Composite stratigraphic section of the Tinton, New Egypt, and Hornerstown Formations near Eatontown, northeastern Monmouth County, showing the distribution of cephalopods and dinoflagellates (nonreworked) with respect to the standard zonation of foraminifera, nannofossils, and ammonites.

Fig. 3 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. 3. Detailed locality map of northeastern Monmouth County, New Jersey, showing the areal extent of the New Egypt Formation (Kne) and its contact with the underlying Tinton formation (Kt) and overlying Hornerstown Formation (Tht). Numbers correspond to those in the list of localities.

Fig. 2 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. 2. Standard stratigraphic sequence of part of the Upper Cretaceous and Lower Tertiary succession in Monmouth County, New Jersey (reproduced from Olsson, 1987). In earlier interpretations (Olsson, 1963), the New Egypt Formation was also considered to be equivalent to parts of the Hornerstown and Navesink formations.

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Data for Nemes et al. "Springing forward: Migrating songbirds catch up with the start of spring in North America"

<p>R scripts and data used to estimate bird migration rate and timing relative to spring onset rate and timing within North America.</p>

Fig. 111. Dorsoventral cross section through a in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 111. Dorsoventral cross section through a small microconch of Hoploscaphites brevis (Meek, 1876), transitional in morphology to macroconch, BHI 4248, Baculites compressus–B. cuneatus zones, Pierre Shale, Meade County, South Dakota. The plane of the cross section approximately coincides with the line of maximum length. A. Camera lucida of cross section of the adult shell. The stippled area demarcates the mature body chamber. B. Camera lucida of cross section of the inner whorls. C. Photo of cross section of the inner whorls. Measurements are listed in appendix 2, table 4.

Fig. 115 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 115. Ontogenetic breakdown of Hoploscaphites brevis (Meek, 1876), macroconch, USNM 536238, locality unknown, but probably Pierre Shale, Meade or Pennington County, South Dakota. A–F. Six sizes through ontogeny in lateral and ventral views showing changes in ornamentation from early ontogeny (F) to maturity (A).

Fig. 107 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 107. Hoploscaphites brevis (Meek, 1876), small microconchs. A–D. BHI 4245, Baculites cuneatus Zone, Pierre Shale, Meade County, South Dakota. A. Right lateral; B. apertural; C. ventral; D. left lateral. E–H. BHI 4253, transitional in morphology to macroconch, Baculites compressus Zone, Pierre Shale, Meade County, South Dakota. E. Right lateral; F. apertural; G. ventral; H. left lateral. I–L. BHI 2155, Baculites compressus Zone, Pierre Shale, Meade County, South Dakota. I. Right lateral; J. apertural; K. ventral; L. left lateral. M–P. BHI 4276, Baculites compressus–B. cuneatus zones, Pierre Shale, Meade County, South Dakota. M. Right lateral; N. apertural; O. ventral; P. left lateral. Specimens are illustrated natural size.

Fig. 97 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 97. Hoploscaphites brevis (Meek, 1876), small macroconchs. A–D. BHI 4796, Baculites compressus–B. cuneatus zones, Pierre Shale, Meade County, South Dakota. A. Right lateral; B. apertural;

Fig. 94 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 94. Hoploscaphites brevis (Meek, 1876), large macroconchs. A, B. BHI 4789, Baculites compressus– B. cuneatus zones, Pierre Shale, Pennington County, South Dakota. A. Right lateral; B. ventral. C, D. USNM 536221, USGS Mesozoic loc. 22182, Baculites compressus–B. reesidei zones, Bearpaw Shale, Fergus County, Montana. C. Right lateral; D. ventral. A piece of shell is missing from the adapical part of the body chamber. Specimens are illustrated natural size.

Fig. 96 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 96. Hoploscaphites brevis (Meek, 1876), small macroconchs. A–C. BHI 4274, Baculites cuneatus Zone, Pierre Shale, Meade County, South Dakota. A. Apertural; B. ventral; C. left lateral. D–F. BHI 4292,

Fig. 90 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 90. Hoploscaphites brevis (Meek, 1876), large macroconch, AMNH 56882, AMNH loc. 3436, Baculites compressus Zone, Pierre Shale, Meade County, South Dakota. A. Right lateral; B. apertural; C. ventral; D. left lateral. Specimen is illustrated natural size.

Fig. 93 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 93. Hoploscaphites brevis (Meek, 1876), large macroconchs. A, B. AMNH 63442, slightly distorted, Pierre Shale, near Kremmling, Grand County, Colorado. The position of the base of the body chamber is estimated. A. Ventral; B. left lateral. C, D. BHI 4910a, very similar to holotype, Baculites compressus–B. cuneatus zones, Pierre Shale, Pennington County, South Dakota. C. Ventral; D. left lateral. Specimens are illustrated natural size.

Fig. 89 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 89. Hoploscaphites brevis (Meek, 1876), large macroconchs. A–C. BHI 4124, Baculites compressus– B. cuneatus zones, Pierre Shale, Meade County, South Dakota. A. Right lateral; B. apertural; C. ventral. D–F. BHI 4202, Baculites compressus Zone, Pierre Shale, Meade County, South Dakota. D. Apertural; E. ventral; F. left lateral. Specimens are illustrated natural size.