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(Tab. 2) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 1-4, Blake-Bahama Basin

Name: (Tab. 2) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 1-4, Blake-Bahama Basin
Creator: Riegraf, Wolfgang; Luterbacher, Hanspeter
Published: 1989-01-01T00:00:00+08:00

PANGAEA1989-01-01 更新2026-04-09 收录

海洋环境重建

底栖有孔虫生物地层

数据链接：

https://doi.pangaea.de/10.1594/PANGAEA.668228 数据链接链接失效反馈

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资源简介：

C = common, R = rare, - = absent. Lithology: nannoplankton chalk

应用场景：

提供机构：

Riegraf, Wolfgang; Luterbacher, Hanspeter

创建时间：

1989-01-01

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Stable oxygen isotopic ratios in corals (d18Ocoral) are commonly utilized to reconstruct climate variability beyond the limit of instrumental observations. These measurements provide constraints on pa

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Relative abundance of coccosphere-units at site GIK23414

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Age given in calendar years. Coccosphere-unit: Conversion of coccoliths to hypothetical coccospheres by taking an average number of coccoliths per coccosphere.

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(Table 6) Ranges of benthic foraminifers through the Oligocene in DSDP Hole 2...

底栖有孔虫生物地层

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Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because...

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Supplementary material Supplementary material Table 1, Taxonomic information of total radiolarian taxa encountered in study. Supplementary material Table 2, Basic environmental informations with annua

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We use a multiproxy approach to monitor changes in the vertical profile of the Indonesian Throughflow as well as monsoonal wind and precipitation patterns in the Timor Sea on...

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(Tab. 2) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 1-4, Blake-Bahama Basin

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