Distribution of calcareous nannofossils in the sparopel layers of hole 69-2SL, Meteor cruise 40/4, Eastern Mediterranean Sea.

Journal of Nannoplankton Research Pub Date : 1900-01-01 DOI:10.58998/jnr2096

D. Frydas, Christoph Hemlebent, Spyridōn, Bellas

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Abstract

Calcareous nannoplankton associations from the sapropel layers of the gravity core M40/4, Station 69-2L, south-eastern Mediterranean Sea, have been examined. The investigated core mainly consists of nannofossil-/foraminifera-bearing mud, sapropel layers SI to SS/6 (except S2), and tephra layers. A subtropical coccolitb association was recognised in sapropels SI, S4, SS, SS/6, while a temperate one characterises S3. A reversal in dominance between Gephyrompse< muelleme and Emilie

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东地中海流星巡航40/4号69-2SL孔稀疏层中钙质纳米化石的分布

研究了地中海东南部69-2L站M40/4重力岩心的浅水推进层中钙质纳米浮游生物的组合。研究的岩心主要由含纳米化石/有孔虫的泥、SI ~ SS/6 (S2除外)的泥推进层和泥层组成。SI、S4、SS、SS/6的球粒岩属于亚热带球粒岩组合，S3属于温带球粒岩组合。在深度256cm的S3层，Gephyrompse< muelleme和Emilie

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