FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1984702903> ?p ?o ?g. }

• W1984702903 endingPage "400" @default.
• W1984702903 startingPage "391" @default.
• W1984702903 abstract "Abstract Despite high taxonomic diversity elsewhere in North America during the Pleistocene, vertebrate faunas are exceedingly rare in the region of northern Mexico. Terapa, a unique fossil site located in the present-day desert of Northcentral Sonora, Mexico (29°41′N, 109°39′W, 605 m elevation), contributes to our understanding of the paleoecology and paleoclimate of the region during the Late Pleistocene, ca. 43,000–40,000 cal. yr BP. At least 60 vertebrate taxa, including amphibians, turtles, a crocodilian, snakes, birds and many mammals, have been recovered from an 11-m thick sequence of fossiliferous sediments. The diversity and tropical affinity of these taxa suggest a more-forested environment than the thornscrub desert habitat present in this region today. Isotopic analyses of tooth enamel carbonate from ancient mammalian herbivores suggest that the Sonoran desert has undergone considerable climate change since the Late Pleistocene. Bulk carbon (δ13C) and oxygen (δ18O) isotopes from nine mammalian fossils indicate a habitat mosaic with variations in diet that include browsers, mixed feeders and C4 hyper-grazers (δ13C range of − 10‰ to 2‰). Unique to this site are δ13C tooth enamel values of − 6.1 and − 5.6 ‰ for the deer Odocoileus, which suggest a more variable diet than strict browsing, including possibly feeding on CAM and/or C4 plants. Serial sampling of carbon (δ13C) and oxygen (δ18O) isotopes for ancient mammal teeth with hypsodont dentitions (fossil Equus and Bison,) as well as δ18O meteroric water estimates from well-supported climatic models suggest a cooler and more equable environment at Terapa during the Late Pleistocene. These results also support previous habitat reconstructions inferred from the macrobotanical and packrat midden records of northern Sonora (Mexico). High-resolution stable isotope geochemistry indicates that: 1) ancient Terapa was covered with forest and grassland habitats that extended northward into Mexico by about 350 km relative to their present-day northern limits during the Late Pleistocene; and 2) an Amount Effect (AE) is demonstrated in the fossil record at Terapa even though the climate was less seasonal compared to the modern desert habitat." @default.
• W1984702903 created "2016-06-24" @default.
• W1984702903 creator A5013404599 @default.
• W1984702903 creator A5015206706 @default.
• W1984702903 creator A5061903711 @default.
• W1984702903 creator A5070628824 @default.
• W1984702903 date "2010-11-01" @default.
• W1984702903 modified "2023-10-01" @default.
• W1984702903 title "Ancient forests and grasslands in the desert: Diet and habitat of Late Pleistocene mammals from Northcentral Sonora, Mexico" @default.
• W1984702903 cites W111488047 @default.
• W1984702903 cites W1610719105 @default.
• W1984702903 cites W1675802314 @default.
• W1984702903 cites W1968322660 @default.
• W1984702903 cites W1970884565 @default.
• W1984702903 cites W1971490401 @default.
• W1984702903 cites W1973326864 @default.
• W1984702903 cites W1978485565 @default.
• W1984702903 cites W1984875825 @default.
• W1984702903 cites W1988378253 @default.
• W1984702903 cites W1996921359 @default.
• W1984702903 cites W1999241836 @default.
• W1984702903 cites W2004870462 @default.
• W1984702903 cites W2006684236 @default.
• W1984702903 cites W2008281306 @default.
• W1984702903 cites W2010328480 @default.
• W1984702903 cites W2016408837 @default.
• W1984702903 cites W2019908571 @default.
• W1984702903 cites W2020184445 @default.
• W1984702903 cites W2032855124 @default.
• W1984702903 cites W2034288750 @default.
• W1984702903 cites W2037258776 @default.
• W1984702903 cites W2042691702 @default.
• W1984702903 cites W2063987912 @default.
• W1984702903 cites W2064112126 @default.
• W1984702903 cites W2070949904 @default.
• W1984702903 cites W2083659742 @default.
• W1984702903 cites W2084458063 @default.
• W1984702903 cites W2084954343 @default.
• W1984702903 cites W2086119112 @default.
• W1984702903 cites W2092041880 @default.
• W1984702903 cites W2099762554 @default.
• W1984702903 cites W2103276374 @default.
• W1984702903 cites W2103599000 @default.
• W1984702903 cites W2131091648 @default.
• W1984702903 cites W2133931239 @default.
• W1984702903 cites W2137725470 @default.
• W1984702903 cites W2142828220 @default.
• W1984702903 cites W2143804637 @default.
• W1984702903 cites W2155248601 @default.
• W1984702903 cites W2156765492 @default.
• W1984702903 cites W2168813320 @default.
• W1984702903 cites W2171022590 @default.
• W1984702903 cites W2174329518 @default.
• W1984702903 cites W2178515861 @default.
• W1984702903 cites W2178606940 @default.
• W1984702903 cites W2219841968 @default.
• W1984702903 cites W2316123839 @default.
• W1984702903 cites W2328527260 @default.
• W1984702903 cites W4238980658 @default.
• W1984702903 cites W2036887504 @default.
• W1984702903 doi "https://doi.org/10.1016/j.palaeo.2010.08.021" @default.
• W1984702903 hasPublicationYear "2010" @default.
• W1984702903 type Work @default.
• W1984702903 sameAs 1984702903 @default.
• W1984702903 citedByCount "42" @default.
• W1984702903 countsByYear W19847029032012 @default.
• W1984702903 countsByYear W19847029032013 @default.
• W1984702903 countsByYear W19847029032014 @default.
• W1984702903 countsByYear W19847029032015 @default.
• W1984702903 countsByYear W19847029032016 @default.
• W1984702903 countsByYear W19847029032017 @default.
• W1984702903 countsByYear W19847029032019 @default.
• W1984702903 countsByYear W19847029032020 @default.
• W1984702903 countsByYear W19847029032021 @default.
• W1984702903 countsByYear W19847029032022 @default.
• W1984702903 countsByYear W19847029032023 @default.
• W1984702903 crossrefType "journal-article" @default.
• W1984702903 hasAuthorship W1984702903A5013404599 @default.
• W1984702903 hasAuthorship W1984702903A5015206706 @default.
• W1984702903 hasAuthorship W1984702903A5061903711 @default.
• W1984702903 hasAuthorship W1984702903A5070628824 @default.
• W1984702903 hasConcept C111472728 @default.
• W1984702903 hasConcept C138885662 @default.
• W1984702903 hasConcept C166957645 @default.
• W1984702903 hasConcept C185933670 @default.
• W1984702903 hasConcept C18903297 @default.
• W1984702903 hasConcept C205649164 @default.
• W1984702903 hasConcept C2776130869 @default.
• W1984702903 hasConcept C53570757 @default.
• W1984702903 hasConcept C86803240 @default.
• W1984702903 hasConceptScore W1984702903C111472728 @default.
• W1984702903 hasConceptScore W1984702903C138885662 @default.
• W1984702903 hasConceptScore W1984702903C166957645 @default.
• W1984702903 hasConceptScore W1984702903C185933670 @default.
• W1984702903 hasConceptScore W1984702903C18903297 @default.
• W1984702903 hasConceptScore W1984702903C205649164 @default.
• W1984702903 hasConceptScore W1984702903C2776130869 @default.
• W1984702903 hasConceptScore W1984702903C53570757 @default.

• next