Dataset - B2FIND

High-resolution census data of Extinction Group species in the Late Pliocene-...

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(Appendix A2) Distribution of benthic foraminifera in ODP Site 184-1146

Depth, sediment is composite depth (mcd).

(Appendix A) Environmental and foraminiferal proxy data of surface sediments ...

Samples are taken from the top few centimetres

(Appendix A) Stable carbon and oxygen isotopes and paleoproductivity reconstr...

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(Appendix 1) Benthic foraminiferal abundance and diversities of DSDP Hole 90-594

Further relevant data sets: Nelson et al. (1986) doi:10.1594/PANGAEA.688744, Dersch and Stein (1991) doi:10.1594/PANGAEA.667464, Dudley and Nelson (1994)...

(Appendix 1) Environmental proxy data of ODP Site 90-594

Further relevant data sets: Nelson et al. (1986) doi:10.1594/PANGAEA.688744, Dersch and Stein (1991) doi:10.1594/PANGAEA.667464, Dudley and Nelson (1994)...

Benthic and planktic foraminiferal data of sediment core PS93/016

This dataset shows benthic and planktic foraminiferal data, planktic foraminiferal fragmentation and coarse fraction values. The sampled sediment record PS93/016, consisting of...

Pliocene benthic foraminiferal abundances of ODP Hole 105-646B from north Atl...

Our benthic foraminiferal data clearly indicate eight layers of deep-water turbidites during the Messinian (MTL 1-8) and one in the early Pliocene (PTL 1) in Ocean Drilling...

Benthic and planktic foraminiferal Mg/Ca, Ba/Ca and local seawater d18O estim...

During the middle Miocene, Earth's climate changed from a global warm period (Miocene Climatic Optimum) into a colder one with the expansion of the Antarctic ice sheet. This...

Dissolution proxy and isotopic data for IODP Site 1262B (Leg 208)

This data set presents results obtained from isotopes of carbon and oxygen. Results are also presented regarding the content of calcium carbonate (CaCO3 %). Dissolution proxies...

Planktonic foraminifera of sediment core CDH-79

D= dominant (>30%), A= abundant (10%–30%), F= few (5%–10%), R= rare (1%–5%), P= present (<1%), and B= barren (no planktonic foraminifers).

(Table 1) Planktonic foraminiferal abundance at DSDP Site 94-606

A "total fauna" curve (Ruddiman, 1971; doi:10.1130/0016-7606(1971)82[283:PSITEA]2.0.CO;2) shows that surface water overlying DSDP Site 606 (central North Atlantic Ocean) cooled...

Size normalized planktic foraminifera weight and coccolith diameter from DSDP...

As a result of anthropogenic pCO2 increases, future oceans are growing warmer and lower in pH and oxygen, conditions that are likely to impact planktic communities. Past...