Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
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约旦河谷 Qeren Sartaba 早至中始新世的介形类和有孔虫
DOI：
10.1144/jm.10.1.95
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发表时间：
1991
影响因子：
2
通讯作者：
C. Benjamini
中科院分区：
文献类型：
--
作者：
A. Honigstein;A. Rosenfeld;C. Benjamini
描述和说明了来自约旦河谷中部 80 m 厚的 Qeren Sartaba 剖面的 23 种介形类和 20 个浮游有孔虫物种和物种组。经浮游有孔虫生物地层学测定，该物质属于早始新世晚期（P9带上部）和中始新世早期（P10带）。古生态学是中上层海洋陆架的代表，具有周期性的浅化和硬地形成事件。
23 species of ostracods and 20 species and species groups of planktonic foraminifera from the 80m thick Qeren Sartabasection, central Jordan Valley, are described and illustrated. The material is determined by planktonic foraminiferal biostratigraphy to belong to the latest Early Eocene (upper part of Zone P9) and the early Middle Eocene (Zone P10). The palaeoecology is representative of a pelagic marine shelf, with periodic events of shallowing and hardground formation.