MIOCENE-PLIOCENE BOUNDARY IN PHILIPPINES AS RELATED TO LATE TERTIARY STRATIGRAPHY OF DEEP-SEA SEDIMENTS
MIOCENE-PLIOCENE BOUNDARY IN PHILIPPINES AS RELATED TO LATE TERTIARY STRATIGRAPHY OF DEEP-SEA SEDIMENTS
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DOI：
10.1126/science.142.3597.1290
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发表时间：
1963-01-01
期刊：
影响因子：
56.9
通讯作者：
BANDY, OL
中科院分区：
文献类型：
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作者：
BANDY, OL
菲律宾中新世-上新世界线上的浮游有孔虫趋势表明，据报道为上新世的8个深海岩心的剖面实际上是最晚的中新世，深海岩心中的discoasters明显灭绝是由于不整合，分离了中新世和更新世沉积物，代表上新世时间的约1000万年的时间差距。整个中新世的浮游有孔虫趋势-菲律宾的上新世界线表明，据报道为上新世的8个深海岩心的剖面实际上是中新世晚期，深海岩心中的discoasters明显灭绝是由于不整合，分离了中新世和更新世沉积物，代表着上新世大约1000万年的时间间隔。
Planktonic foraminiferal trends across the Miocene-Pliocene boundary in the Philippines suggest that sections of eight deep-sea cores reported to be Pliocene are actually latest Miocene, and that a marked extinction of discoasters in the deep-sea cores is due to an unconformity, separating Miocene and Pleistocene sediments, representing a time gap of some 10 million years of Pliocene time.Planktonic foraminiferal trends across the Miocene-Pliocene boundary in the Philippines suggest that sections of eight deep-sea cores reported to be Pliocene are actually latest Miocene, and that a marked extinction of discoasters in the deep-sea cores is due to an unconformity, separating Miocene and Pleistocene sediments, representing a time gap of some 10 million years of Pliocene time.