Late Cainozoic Ostracoda from Deep Sea Drilling Project Leg 31(Site 296)
Gou Yunxian
Abstract
Gou Yunxian
Abstract
Eleven benthonic ostracod species belonging to eight genera were encountered in core samples ranging in age from the Pliocene to the Holocene of Site 296 of DSDP Leg 31. Almost all the modern descendants of the genera and known species in this study are abyssal inhabitants and their fossil records also originate from the deep-sea sediments in the world ocean during the Cainozoic. The discovery of deep-sea (psychrospheric) ostracods in the studied area indicates that during the Quaternary in the marginal northwestern Pacific, an abyssal depth existed probably as deep as that of the present day, but greater than that in the Pliocene.
OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Eleven benthonic ostracod species belonging to eight genera were encountered in core samples ranging in age from the Pliocene to the Holocene of Site 296 of DSDP Leg 31. Almost all the modern descendants of the genera and known species in this study are abyssal inhabitants and their fossil records also originate from the deep-sea sediments in the world ocean during the Cainozoic. The discovery of deep-sea (psychrospheric) ostracods in the studied area indicates that during the Quaternary in the marginal northwestern Pacific, an abyssal depth existed probably as deep as that of the present day, but greater than that in the Pliocene.
Key concepts: Abyssal zone, Cenozoic, Deep sea, Ostracod, Geology, Quaternary, Paleontology, Abyssal plain