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(Table 4) Benthic foraminiferal community at DSDP Hole 94-609B
This dataset has no description
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(Table 4) Oxygen and carbon isotopic composition of benthic foraminifers at D...
This dataset has no description
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(Table 2) Oxygen and carbon isotopic composition of benthic foraminifers at D...
This dataset has no description
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(Table 2) Planktonic foraminifera community at DSDP Hole 94-610
VR = very rare, R = rare, C = common, A = abundant, X = reworked, cf. = compare, - = absent. -
(Table 1) Planktonic foraminifera community at DSDP Hole 94-608
VR = very rare, R = rare, C = common, A = abundant, X = reworked, cf. = compare, - = absent. -
(Appendix D) Benthic foraminifera extinction group species in DSDP Hole 94-608
This dataset has no description
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Relative abundances of dinoflagellate cysts in several IODP and DSDP holes
This dataset has no description
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Raw counts of dinoflagellate cysts in several IODP and DSDP holes
This dataset has no description
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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... -
(Table 1) Planktonic foraminiferal communities at DSDP Holes 94-609B and 94-609
The planktonic foraminifers in 124 samples from Holes 609 and 609B have been analyzed quantitatively to see whether oceanographic events in the late Miocene and early Pliocene... -
(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... -
Distribution of calcareous nannofossils in the Miocene interval of DSDP Hole ...
DSDP North Atlantic Site 608 yielded an excellent Miocene pelagic section which affords a further opportunity for elucidating the chronology of the calcareous nannofossil... -
Dinoflagellate cyst abundances at DSDP Site 94-607 from the North Atlantic (A...
The climatic deterioration related to the onset of Northern Hemisphere glaciations (circa 2.52 Ma BP) must have lead to reorganization and relocation of species associations and... -
Planktic foraminifera abundance of Hole 94-611E
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 94-611D
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 94-611C
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 94-611A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 94-611
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 94-610E
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 94-610D
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
