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(Table 1) Oxygen- and carbon-isotopes of Globigerina bulloides and Neogloboqu...
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(Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP...
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Mg/Ca ratios of Cibicidoides robertsonianus and BWT reconstruction of DSDP Ho...
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(Fig. 13) Distribution of dinoflagellate cysts in Early Cretaceous sediments ...
Species abundance: F = 1-5 %, C = 6-15 %, A = >15 %, - = not present -
(Figure 1) Dinoflagellate cyst stratigraphy of DSDP Hole 80-548A
Cyst assemblages from Sites 548, 549, and 550 were examined and gave evidence of early Eocene to late Miocene age. These assemblages were compared with other North Atlantic... -
(Table 3) Oxygen isotope ratios of benthic foraminifera from DSDP Hole 80-548
Presently, the intermediate depths of the North Atlantic Ocean are occupied by a great lens of warm, saline water whose source is the Mediterranean Sea. This water flows both... -
Late Pliocene sea-surface temperature record of DSDP Hole 80-548 from the Nor...
Application of quantitative micropaleontologic methods of sea-surface temperature (SST) estimation to the planktic foraminiferal faunas at Hole 548 in the northeast Atlantic... -
(Appendix) Late Cretaceous calcareous nannofossils of DSDP Holes 80-549 and 8...
he early late Cretaceous (Cenomanian–early Turonian) is thought to have been one of the warmest periods of the Phanerozoic. This period was characterised by tropical sea surface... -
Chronostratigraphic summary for Middle Miocene through Pliocene dinoflagellat...
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Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(Table 4) Morphologic variability in the Globorotalia puncticulata group and ...
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(Table 3) Globorotalia puncticulata, Globorotalia inflata, and their intergra...
Number of chambers in final chamber set are as seen from spiral side, 3 = 3 to 3.75, 4 = 4 to 4.5. -
(Table 2) Planktonic foraminiferal abundances in samples spanning the first a...
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Morphometric study of porosity and morphology of fossil Globigerinoides, Chp4...
Nomenclature of each specimen follows the rule described in Annex 1.1. Images are grouped following the original file names used during this work: thus, the number of the “GEO”... -
Nd-iostope composition of DSDP Hole 80-548
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(Table 1b) Marine Osmium records during the late Paleocene thermal maximum in...
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(Table S3) Comparison of the magnitude of the CIEs of PETM, ETM2 and H2 in th...
Asterisk (*) denotes incomplete sequence. -
(Table S2) Linear sedimentation rates preceding and following ETM2 in the Atl...
A significant post-ETM2 reduction is observed everywhere. Sites with () symbols provide estimates while Sites with (*) provide different approximations, based on different age... -
Median grain sizes and percentage of sortable silt of DSDP Site 80-550
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