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GTS-12 adjusted age models for DSDP Site 72-516
GTS-12 timescale adjusted age models for DSDP site 516 with biostratigraphic (calcareous nannoplankton and foraminifer) and magnetostratigraphic datums. -
Cenozoic TEX86-derived global SST compilation including new data from ODP/DSD...
Cenozoic global TEX86-derived sea surface temperature (SST) compilation from all published marine TEX86 records and new data measured in this study (ODP/DSDP Sites 516, 588,... -
Noelaerhabdaceae coccolith length (mean, 5th percentile and 95th percentile) ...
This dataset contains the data plotted in Figure 5 of the review paper Coccoliths as Recorders of Paleoceanography and Paleoclimate over the Past 66 Million Years by Bolton... -
Sea surface temperature anomalies for Pliocene interglacial KM5c (PlioVAR)
We examine a single interglacial during the late Pliocene (KM5c, ca. 3.205 +/- 0.01 Ma) when atmospheric CO2 concentrations were higher than pre-industrial, but similar to today... -
(Table S1) Nannofossil relative abundance and flux for DSDP Sites 72-516
This dataset has no description
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(Figure 3) Occurrence of diatoms at DSDP Hole 72-516F
Counts indicate the number of specimens observed in two traverses of 22 x 22 mm cover slip at x 400; #11 = 11 to 50 specimens observed in two traverses. -
(Figure 1) Occurrence, abundance, and preservation of diatoms at DSDP Hole 72...
Diatom abundances: P = present, r = present but suspected reworking, - = absent. ln Sample 72-515B-50-4,100-120 there is a trace of pyritized diatoms. -
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... -
(Appendix) Ostracodes at DSDP Leg 72 Holes
From the study of the ostracodes of Sites 516, 517, and 518 in comparison with those of Sites 21, 22, and 357, we can show that a time lag (early to late Oliogene) existed... -
(Appendix) Benthic foraminifera distribution of upper Creatceous and Paleocen...
Benthic foraminifers of the Coniacian-Santonian through the Paleocene were recovered from a continuous pelagic carbonate section from Hole 516F on the Rio Grande Rise.... -
Vertical distribution of nannofossils in the section of DSDP Site 72-516
Calcareous nannoplankton from 44 samples of a thick (169.5 m) Neogene section of DSDP Site 516 in the South Atlantic was studied. More than 60 species were determined.... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
Rare Earth Element concentrations of bulk sediment leachates at DSDP Site 72-...
This dataset includes the analysis of sediment core DSDP 517 (30°56.81'S, 38°02.47'W, 2963 m water depth) recovered from the Rio Grande Rise within the modern day North Atlantic... -
Rare Earth Element concentrations of bulk sediment leachates at DSDP Site 72-...
This dataset includes the analysis of sediment core DSDP 516 (30°16'S, 35°17'W, 1313 m water depth) recovered from the Rio Grande Rise within the modern day core of Antarctic... -
(Appendix B) Distribution of planktonic foraminifera at DSDP Hole 72-518
Numbers have been rounded to the nearest percent. -
(Appendix A) Distribution of planktonic foraminifera at DSDP Hole 72-516
Numbers have been rounded to the nearest percent. -
(Table 2) Benthic foraminifers at DSDP Hole 72-515A
This dataset has no description
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(Figure 2) Quaternary biostratigraphy and planktonic foraminifera of DSDP Hol...
Sediment depth is given in mbsf. Species abundance: R= rare, F = few, C = common, A = abundant, - = absent. -
(Table 4) Occurrence of benthic foraminifera in samples from DSDP Hole 72-518
This dataset has no description
