机译:中生代海洋缺氧事件过程中光区共济条件的发展的进一步证据
Organic Geochemistry Unit, Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK (e-mail: R.D.Pancost@bristol.ac.uk);
Organic Geochemistry Unit, Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK (e-mail: R.D.Pancost@bristol.ac.uk);
Organic Geochemistry Unit, Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK (e-mail: R.D.Pancost@bristol.ac.uk);
Organic Geochemistry Unit, Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK (e-mail: R.D.Pancost@bristol.ac.uk);
Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK;
Organic Geochemistry Unit, Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK (e-mail: R.D.Pancost@bristol.ac.uk);
13C/12C; Jurassic; Cretaceous; maleimides; oceanic anoxic events;
机译:在中生代海洋缺氧事件中形成光合带共济条件的进一步证据
机译:在Toarcian海洋缺氧事件中,在欧洲大陆架边缘(Pieniny Klippen Belt,斯洛伐克)附近发生了富营养化条件和高硫埋葬
机译:Photic-Zone exinia和缺氧事件在深层Demonian Shelfal海上披肩大陆山脉,NW Canada:改变了德文郡海洋和海平面波动的范式
机译:陆上哥伦比亚东部和北部的白垩纪海洋缺氧事件的沉积学表达
机译:温室气候条件下的有机碳埋藏:西部内部海道内晚白垩世海洋缺氧事件3的区域表达
机译:铀同位素证据表明在海洋缺氧事件2中发生了两次脱氧
机译:北部特提斯中上层海域海洋缺氧事件2中有氧条件的证据
机译:海洋地壳内部结构的多通道地震图像:中生代中大西洋海脊下岩浆室的证据