Disentangling the control of tectonics, eustasy, trophic conditions and climate on shallow-marine carbonate production during the Aalenian-Oxfordian interval: From the western France platform to the western Tethyan domain
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- 作者：Simon Andrieua ; simon.andrieu@u-psud.fr" class="auth_mail" title="E-mail the corresponding author ; Benjamin Brigauda ; Jocelyn Barbaranda ; Eric Lasseurb ; Thomas Saucè ; dec
- 关键词：Carbonate platform ; Facies ; Sequence stratigraphy ; Tectonics ; Jurassic
- 刊名：Sedimentary Geology
- 出版年：2016
- 出版时间：November 2016
- 年：2016
- 卷：345
- 期：Complete
- 页码：54-84
- 全文大小：12641 K
文摘
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Carbonate platform evolution was reconstructed along a 500 km cross-section.
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Tectonism triggered two major phases of rise and fall in carbonate production.
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Basement topography acted as a major control over lateral variations of paleodepth.
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Photozoan carbonate production was promoted by dry climate and low nutrient input.
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Wet climate and eutrophication of epeiric seas lead to low carbonate production.
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