Find research datasets worth reusing

Fig. 83 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 83. Prionocyclus wyomingensis Meek,

Fig. 95 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 95. Prionocyclus novimexicanus (Marcou, 1858). USNM 498422; see also figure 94. Reduced

Fig. 39 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 39. Collignoniceras praecox (Haas, 1946), gracile form. A–C. USNM 498268; D–F. USNM

Fig. 25 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 25. Collignoniceras woollgari regulare (Haas, 1946). USNM 498248, robust form from locality

Fig. 21 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 21. Collignoniceras woollgari regulare (Haas, 1946). A, B. USNM 498239, gracile form. C,

Fig. 13 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 13. Collignoniceras woollgari woollgari (Mantell, 1822). USNM 498216, from locality 48.

Fig. 24 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 24. Collignoniceras woollgari regulare (Haas, 1946). USNM 420012, robust form from locality

Fig. 6 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 6. Cibolaites molenaari Cobban and Hook, 1983. A–C. Paratype USNM 328761, a gracile

Fig. 4 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 4. Measurements used in the text: D = diameter, Wb = whorl breadth, Wh = whorl height, U

Fig. 2 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 2. Turonian ammonite zonation used in the text, based on Cobban (1984a), Kennedy et al.

Fig. 3 in A Revision Of The Turonian Members Of The Ammonite Subfamily Collignoniceratinae From The United States Western Interior And Gulf Coast

Fig. 3. Stratigraphic distribution of Collignoniceratinae in the U.S. Western Interior.

publicOct 2019View details →

dryad36/100

Data from: The first skeletal record of the enigmatic Cretaceous sawfish genus Ptychotrygon (Chondrichthyes, Batoidea) from the Turonian of Morocco

Open the record for dataset details and reuse information.

zenodo32/100

text-fig. 6. Skull reconstructions of representatives of Cretaceous OTUs in left lateral view, a, abelisaurid Camotaurus sastrei, Late Cretaceous (Campanian), Gorro Frigio Formation, Argentina; based on Bonaparte et al. (1990) and MACN CH 894. b, composite skull of a generalized baryonychid; mainly based on Suchomimus tenerensis (MNN GDF 501, 503-506) and Irritator challenged (SMNS 58022), with some elements reconstructed after Baryonyx walkeri (BMNH R 9951). c, carcharodontosaurid Carcharodontosaurus sahariens, Late Cretaceous (Cenomanian), Kem Kem beds, Morocco; based on Sereno et al. (1996) and SGM-Din 1, unpreserved elements shaded. D, dromaeosaurid Velociraptor mongoliensis, Late Cretaceous (Campanian), Djadokhta Formation, Mongolia; based on Barsbold (1983), Barsbold and Osmólska (1999), and AMNH 6515. e, ornithomimosaur Dromiceiomimus brevitertius, Late Cretaceous (Maastrichtian), Horseshoe Canyon Formation, Alberta, Canada; redrawn from Russell (1972). F, oviraptorosaur Oviraptor philoceratops, Late Cretaceous (Campanian), Djadokhta Formation, Mongolia; redrawn from Barsbold et al. (1990). G, therizinosauroid Erlikosaurus andrewsi, Late Cretaceous (Cenomanian- Turonian), Baynshiren Svita, Mongolia; based on Clark et al. (1994). H, tyrannosaurid Gorgosaurus libratus, Late Cretaceous (Campanian), Judith River Formation, Alberta, Canada, redrawn from Molnar et al. (1990). Abbreviations as in Text-figures 4 and 5, and: acc. op., accessory opening of unknown function in the premaxilla of Oviraptor (Barsbold et al. 1990); amf, anterior maxillary foramen; pn, pneumatic openings. Scale bars represent 50 mm (d-g) and 100 mm (a-c, h). in The interrelationships and evolution of basal theropod dinosaurs

text-fig. 6. Skull reconstructions of representatives of Cretaceous OTUs in left lateral view, a, abelisaurid Camotaurus sastrei, Late Cretaceous (Campanian), Gorro Frigio Formation, Argentina; based on Bonaparte et al. (1990) and MACN CH 894. b, composite skull of a generalized baryonychid; mainly based on Suchomimus tenerensis (MNN GDF 501, 503-506) and Irritator challenged (SMNS 58022), with some elements reconstructed after Baryonyx walkeri (BMNH R 9951). c, carcharodontosaurid Carcharodontosaurus sahariens, Late Cretaceous (Cenomanian), Kem Kem beds, Morocco; based on Sereno et al. (1996) and SGM-Din 1, unpreserved elements shaded. D, dromaeosaurid Velociraptor mongoliensis, Late Cretaceous (Campanian), Djadokhta Formation, Mongolia; based on Barsbold (1983), Barsbold and Osmólska (1999), and AMNH 6515. e, ornithomimosaur Dromiceiomimus brevitertius, Late Cretaceous (Maastrichtian), Horseshoe Canyon Formation, Alberta, Canada; redrawn from Russell (1972). F, oviraptorosaur Oviraptor philoceratops, Late Cretaceous (Campanian), Djadokhta Formation, Mongolia; redrawn from Barsbold et al. (1990). G, therizinosauroid Erlikosaurus andrewsi, Late Cretaceous (Cenomanian- Turonian), Baynshiren Svita, Mongolia; based on Clark et al. (1994). H, tyrannosaurid Gorgosaurus libratus, Late Cretaceous (Campanian), Judith River Formation, Alberta, Canada, redrawn from Molnar et al. (1990). Abbreviations as in Text-figures 4 and 5, and: acc. op., accessory opening of unknown function in the premaxilla of Oviraptor (Barsbold et al. 1990); amf, anterior maxillary foramen; pn, pneumatic openings. Scale bars represent 50 mm (d-g) and 100 mm (a-c, h).

opennotspecifiedMay 2003View details →

opencc-by-4.0Dec 2021View details →

Late Cretaceous (Cenomanian-Turonian) ocean deoxygenation variability in response to idealized orbital configurations

This dataset contains ocean and ocean biogeochemistry outputs (NetCDF files) from modeling experiments with realistic Cenomano-Turonian paleogeography and various set of idealized Earth' orbit confiurations (Eccentricity, Obliquity, Precession) . The set of simulation targets the ocean oxygenation response to variation in orbital parameters (Sarr et al. 2022) . The simulations have been run using the IPSL-CM5A2 General Circulation Model (Sepulchre et al. 2020 - IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations, GMD) and offline version of PISCESv2 model (Aumont et al., 2015 - PISCES-v2: an ocean biogeochemical model for carbon and ecosystem studies, GMD). It includes 6 ocean-atmosphere simulations and 6 ocean biogeochemistry simulations. Data are monthly averages over the last 100 years of the simulations.

opennotspecifiedJul 2017View details →

TABLE 1 in Systematics, palaeoecology and taphonomy of Turonian oysters from the northern Gabon Coastal Basin

TABLE 1. — List of oyster fauna of Libreville.After Lombard (1930),Dartevelle & Freneix (1957), Musavu Moussavou et al. (2013a, 2014a) and the present study.

opencc-by-4.0Dec 2021View details →

Figure 15 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation

Figure 15. Albian, Cenomanian, and Turonian micro-bioevents, their subtypes defined by agglutinated foraminifers, and interpreted bottomwater nutrient regimes in the Lower Saxony Cretaceous as well as in the Subhercynian subbasins. Micro-bioevent subtypes correlate with one or more acmes of specific agglutinated foraminiferal species. Depositional sequences and their stratigraphical relations are from Janetschke et al. (2015: Fig. 6).

opencc-by-4.0Jul 2012View details →

Text-fig. 2. Lithology of basal Upper Cretaceous sediments at Kaňk – Na Vrších (a). 1 – conglomerates; 2 – limestones; 3 – erosional surface with borings and mineralization; 4 – limestone layer with nodule-like bodies; 5 – calcareous claystones. (after Žítt, 1992; slightly modified). in Sabellidae And Serpulidae (Polychaeta, Canalipalpata) From The Locality Kaňk - Na Vrších In Kutná Hora (Upper Cenomanian - Lower Turonian, Bohemian Cretaceous Basin - The Czech Republic)

Text-fig. 2. Lithology of basal Upper Cretaceous sediments at Kaňk – Na Vrších (a). 1 – conglomerates; 2 – limestones; 3 – erosional surface with borings and mineralization; 4 – limestone layer with nodule-like bodies; 5 – calcareous claystones. (after Žítt, 1992; slightly modified).

opencc-by-4.0Jul 2012View details →

Text-fig. 1. Geographical position of Kutná Hora – Kaňk and detailed location of the site "Na Vrších". in Sabellidae And Serpulidae (Polychaeta, Canalipalpata) From The Locality Kaňk - Na Vrších In Kutná Hora (Upper Cenomanian - Lower Turonian, Bohemian Cretaceous Basin - The Czech Republic)

Text-fig. 1. Geographical position of Kutná Hora – Kaňk and detailed location of the site "Na Vrších".

opencc-by-4.0Dec 2016View details →

Fig. 11 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 11: 1-15 Abatomphalus sp.cf. A.intermedius, Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12434; 16-21 Reugotruncana ellissi Brönnimann & Brown 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12426; 22-27 Gansseria gansseri (Bolli 1951), Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12442 (All specimens x 90).