1) oceanic anoxia
大洋缺氧
1.
The Mid-Cretaceous (125~90 Ma) was one of the warmest greenhouse climate periods of the Phanerozoic, and was characterized by extraordinary igneous events, oceanic anoxia, biotic turnovers and mass extinctions, normal superchron, and oceanic red beds.
文中基于对白垩纪中期异常事件的深入解剖和分析,包括大规模海底火山事件、大洋缺氧事件、生物异常更替与绝灭、白垩纪超静磁带、大洋红层出现等,在探讨白垩纪中期各个事件特征基础上,重点阐述异常事件所引起的全球变化及其对海洋、气候的影响;提出异常事件之间的相互关联与反馈机制。
2) Oceanic anoxic event
大洋缺氧事件
1.
Early Toarcian oceanic anoxic event in the Shuanghu area,northern Tibet:Sedimentology,palaeobiology and geochemistry;
藏北双湖地区早Toarcian期大洋缺氧事件:沉积学、古生物学及地球化学特征
2.
In the Cambrian,there occurred successively a series of catastrophic events in the study area,including oceanic anoxic event,turbidity event and tempest event.
湘西北杨家坪处于鄂中碳酸盐台地西缘，寒武纪期间区内先后出现大洋缺氧事件、浊流事件、风暴事件等突发性灾变沉积。
3) Oceanic Anoxic Events
大洋缺氧事件
1.
Cretaceous Oceanic Anoxic Events:Research Progress and Forthcoming Prospects;
白垩纪大洋缺氧事件:研究进展与未来展望
2.
Re-Os isotope tracing and dating of black shales and oceanic anoxic events;
黑色页岩与大洋缺氧事件的Re-Os同位素示踪与定年研究
4) Oceanic Anoxic Events (OAEs)
大洋缺氧事件(OAEs)
5) oceanic anoxic event
海洋缺氧条件
6) biotic response
大洋氧含量
1.
Late Cretaceous biotic response to marine dissolved oxygen content in southern Tibet.;
西藏南部晚白垩世大洋氧含量变化的生物特征
补充资料：低血流性缺氧
低血流性缺氧
又称"循环性缺氧"。缺氧的一个类型。指血循环障碍，向组织中输送氧量减少的一种状态。是由于动脉血流入组织不足或静脉血流不畅所引起。其特点为动脉血氧分压、氧含量、氧容量、血氧饱和度正常，而静脉血内则显著降低。临床表现为局限或全身紫绀。瘀血性缺氧，紫绀更为明显。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条