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Oxygen and carbon isotope compositions of middle Cretaceous vertebrates from North Africa and Brazil: Ecological and environmental significance
Amiot, Romain1,2; Wang, Xu3; Lecuyer, Christophe1; Buffetaut, Eric4; Boudad, Larbi5; Cavin, Lionel6; Ding, Zhongli3; Fluteau, Frederic7; Kellner, Alexander W. A.8; Tong, Haiyan; Zhang, Fusong3; romain.amiot@univ-lyon1.fr
2010-11-10
发表期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
卷号297期号:2页码:439-451
文章类型Article
摘要In order to investigate mid-Cretaceous terrestrial climates of low paleolatitudes, Moroccan, Tunisian and Brazilian vertebrate apatites have been analyzed for their oxygen and carbon isotope compositions of phosphates (delta O-18(p)) and carbonates (delta O-18(c), delta C-18(c)). At each site, coexisting theropod dinosaurs, titanosaurid sauropods, pterosaurs, crocodilians, turtles and fish have distinct delta O-18(p) and delta C-18(c) values reflecting their ecologies, diets and foraging environments. Oxygen isotope compositions of surface waters (delta O-18(w)) estimated from turtle and crocodile delta O-18(p) values range from -5.0 +/- 1.0 parts per thousand to -2.4 +/- 1.0 parts per thousand, which do not differ from mean annual rainwater values occurring today under inter-tropical sub-arid to arid climates. High water temperatures ranging from 21 +/- 6 degrees C to 34 +/- 2 degrees C deduced from fish delta O-18(p) values are in agreement with those published for mid-Cretaceous low latitudes. Temporary or seasonal droughts are inferred from high delta O-18(p) values of lungfish teeth, even though lower reptile delta O-18(p) values suggest the use of distinct and most likely larger or regularly renewed bodies of water. Environmental conditions of the studied low latitude regions during the Aptian-Cenomanian interval were somewhat similar to those experienced today under semi-arid to arid tropical or equatorial climates, but with higher mean surface temperatures than present-day ones. (C) 2010 Elsevier B.V. All rights reserved.
关键词Middle Cretaceous Stable Isotopes Vertebrate Apatite Morocco Brazil
WOS标题词Science & Technology ; Physical Sciences ; Life Sciences & Biomedicine
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关键词[WOS]PREDATOR-PREY RELATIONSHIPS ; BIOGENIC APATITES ; STABLE-ISOTOPES ; BONE PHOSPHATE ; TOOTH ENAMEL ; PALEOECOLOGICAL IMPLICATIONS ; DELTA-O-18 RECORD ; SANTANA FORMATION ; OSTRICH EGGSHELL ; CLIMATE-CHANGE
收录类别SCI
语种英语
WOS研究方向Physical Geography ; Geology ; Paleontology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS记录号WOS:000284340500016
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文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/4511
专题中科院古脊椎所(2000年以后)
通讯作者romain.amiot@univ-lyon1.fr
作者单位1.Univ Lyon 1, CNRS, UMR 5125, F-69622 Villeurbanne, France
2.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Evolutionary Systemat Vertebrates, Beijing 100044, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
4.Ecole Normale Super, Geol Lab, CNRS, UMR 8538, F-75231 Paris 05, France
5.Univ Moulay Ismail, Lab Format Superficielles, Errachidia 52000, Morocco
6.Museum Hist Nat, Dept Geol & Palaeontol, CH-1211 Geneva 6, Switzerland
7.Inst Phys Globe, F-75005 Paris, France
8.Univ Fed Rio de Janeiro, Museo Nacl, Dept Geol & Paleontol, Paleovertebrate Sector, BR-20940040 Rio De Janeiro, Brazil
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Amiot, Romain,Wang, Xu,Lecuyer, Christophe,et al. Oxygen and carbon isotope compositions of middle Cretaceous vertebrates from North Africa and Brazil: Ecological and environmental significance[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2010,297(2):439-451.
APA Amiot, Romain.,Wang, Xu.,Lecuyer, Christophe.,Buffetaut, Eric.,Boudad, Larbi.,...&romain.amiot@univ-lyon1.fr.(2010).Oxygen and carbon isotope compositions of middle Cretaceous vertebrates from North Africa and Brazil: Ecological and environmental significance.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,297(2),439-451.
MLA Amiot, Romain,et al."Oxygen and carbon isotope compositions of middle Cretaceous vertebrates from North Africa and Brazil: Ecological and environmental significance".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 297.2(2010):439-451.
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