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191 results for “Paleoecology”
FIGURE 3 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 3. Stratigraphic profile composite, including all test pit excavations from cross-section a-a' illustrated in Figure 2. 1, indicates a graphic correlation of the stratigraphic units (profiles A-I) and their lenses (e-f). 2, shows the southern wall profile of the excavation of 1985 (A), whereas the A-profile on the extreme lower right, shows the east wall of the same profile. Profiles B-C pertains to the other test pits. Each Roman numeral indicates the arbitrary 10 cm excavation intervals. Depth, dip, and strike are included for the profiles.
FIGURE 15 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 15. Approximation of paleoenvironment conditions through oxygen stable isotopes from Cueva de los Nesofontes test pit D, compared to other circum-Caribbean deposits (modified from Curtis et al., 2001). The grey areas indicate the timeframe of our deposit and its graphical correlation to our data.
Carrillo-Briceño et al. 2018 (raw isotopic data) - Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia)
<p>The file contains the raw isotopic data for the article entitled '<strong>Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia)</strong>'. It includes the correction for the values first produced by our mass spectrometer and how the corrections were proceeded. Several runs were performed and these are detailed with comments and remarks. Any doubt or question about these corrections are welcomed by me, László Kocsis and Torsten Vennemann for discussion or further considerations.</p>
Data from: Westermann Morphospace displays ammonoid shell shape and hypothetical paleoecology
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Testing size-frequency distributions as a method of ontogenetic aging: a life history assessment of hadrosaurid dinosaurs from the Dinosaur Park Formation of Alberta, Canada, with implications for hadrosaurid paleoecology
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Data from: Using three-dimensional geometric morphometric and dental topographic analyses to infer the systematics and paleoecology of fossil treeshrews (Mammalia, Scandentia)
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Paleoecology of naticid-molluscan prey interaction during the Late Jurassic (Oxfordian) in Kutch, India: Evolutionary implications
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Ph.D. dataset. Neanderthal Paleoecology during the Middle Palaeolithic of Northen and Eastern of Iberian Peninsula. Combined analysis of Tooth Wear and Cementochronology
<p>The archives correspond to the databases created and used for the development of the Ph.D.</p> <p>The 'Ph.D. Sample' correspond with the total amount of ungulates teeth studied. Those are organized by regions, sites, species and techniques employed.</p> <p>The sites files (i.e. Arbreda, Teixoneres, Abric Romaní, El Salt and Covalejos) correspond to the tooth wear (meso- and microwear) and cementum analysis over <em>Cervus elaphus, Equus ferus, Equus hydruntinus, Capra pyrenaica </em>and <em>Bos/Bison. </em></p>
Dataset to Clues to mopane resilience from the perspective of Paleoecology
<p>Dataset accomopanying paper on Clues to mopane resilience from the perspective of Paleoecology submitted to Landscape Ecology.</p> <p>The dataset contains paleoecological data from Lake Chiluetse, Mozambique and site data from archaeological surveys: Lithics and Ceramics. </p>
FIGURE 2 in Tyrannosaurus rex from the Upper Cretaceous (Maastrichtian) North Horn Formation of Utah: biogeographic and paleoecologic implications
FIGURE 2. Reconstruction of late Maastrichtian paleogeography, paleoenvironments, and dinosaur biogeography for the Western Interior of North America. A. Paleoenvironments mapped onto paleogeographic and biogeographic data: white = water (Pacific Ocean and Late Cretaceous Interior Seaway); light gray = seasonally moist coastal plain; white stipple = semiarid alluvial plain; gray stipple = semiarid upland, intermontane basins; and dark gray = upland thrust belts and early Laramide uplifts. Known paleogeographic distribution of three herbivorous dinosaurs are indicated as follows: Alamosaurus sanjuanensis occurrences indicated with ■; Leptoceratops gracilis occurrences indicated with a •; and Triceratops horridus occurrences indicated with a A. Numbers denote fossil sites within specific geologic formations. Geologic formations are indicated as follows: 1 = Scollard, 2 = Willow Creek, 3 = Frenchman, 4 = Hell Creek, 5 = Lance, 6 = Evanston, 7 = Laramie, 8 = North Horn, 9 = Denver, 10 = Kirtland Shale, 11 = McRae, 12 = El Picacho, 13 = Javelina. The North Horn Formation is further indicated by a star. Occurrences of fossil taxa are listed in Gillette et al. (1986), Lehman (1987) and Ryan and Russell (2001). B. Known paleogeographic distribution of the theropod Tyrannosaurus rex. Open circles denote occurrences, except for the North Horn Formation, indicated by a star.
Supplement to: Early Cretaceous climate for the southern Tethyan Ocean: insights from the geochemical and paleoecological analyses of extinct cephalopods
<p>One file (excel) containing XRPD results and Table S1-S6 with details of the clumped isotope, stable carbon isotope, and trace elements analyses that refers to the manuscript.</p>
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Allen Brain Atlas
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DANDI Archive for NWB datasets
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International Brain Laboratory public data
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OpenNeuro
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