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Accumulation rates of biogenic components of ODP Hole 154-926B
The multi-proxies (BAR, bio-SiO2 MAR, and CaCO3 MAR) of productivity in Ocean Drilling Program (ODP) Leg 154 Site 926 Hole B (3°43'N, 42°54'W) during the late Miocene. Based on... -
(Table S1) B/Ca ratios and stable isotope record of Nuttallides umbonifera fr...
Size fraction of benthic foraminifera = 150-250 µm. -
(Table S1) Boron isotope and trace element data and reconstructed carbonate s...
The middle Miocene Climatic Optimum (17-15 Ma; MCO) is a period of global warmth and relatively high CO2 and is thought to be associated with a significant retreat of the... -
(Table A1) CaCO3 contents and Sr/Ca ratios in ODP Leg 130, 138 and 154
Strontium/calcium (Sr/Ca) ratios in bulk and foraminiferal calcite have been used to constrain the history of Sr/Ca in the oceans and to evaluate calcite diagenetic alteration.... -
Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926
Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of... -
(Supplement 7) X-ray fluorescence data (Ca, Fe) from ODP Site 154-927 sediments
DEPTH, sediment is given in mbsf. -
(Supplement 6) X-ray fluorescence data (Ca, Fe) from ODP Hole 154-926B sediments
DEPTH, sediment is given in mbsf. -
(Supplement 5) Greyscale values from ODP Hole 154-928B sediments
DEPTH, sediment is given in mbsf. -
(Supplement 4) Depths and revised depths of ODP Site 154-926
DEPTH, sediment is given in mbsf. -
(Supplement 3) Tie points and La2004 tuned ages of ODP Site 154-926
This dataset has no description
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(Supplement 2) Magnetic susceptibility of ODP Site 154-926 sediments
This dataset has no description
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(Supplement 1) Greyscale values from ODP Site 154-926 sediments
This dataset has no description
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(Table 1) Estimated age for the last occurrence of Globoquadrina dehiscens
Ages were transfered to the timscale of Berggren et al. (1995) -
Core scan image analysis corrected for cracks, ODP Hole 154-926C
Drill cores are essential for the study of deep-sea sediments and on-land sites because often no suitable outcrop is available or accessible. These cores form the backbone of... -
(Table 3) Relative depth and age, CaCO3, δ¹⁸O, δ¹³C and Sr/Ca analysis from O...
Interpretations of calcite strontium/calcium records in terms of ocean history and calcite diagenesis require distinguishing the effects on deep-sea calcite sediments of changes... -
XRF data, magnetic susceptibility, greyscale values and revised depths of sed...
The distinctly cyclic sediments recovered during ODP Leg 154 played an important role in constructing the astronomical time scale and associated astro(bio)chronology for the... -
Late Miocene development of the western Pacific warm pool: Planktonic foramin...
The disappearance at ~10 Ma of the deep dwelling planktonic foraminifer Globoquadrina dehiscens from the western Pacific including the South China Sea was about 3 Myr earlier... -
Middle to late Eocene carbonate accumulation rates of ODP Hole 154-929E
This dataset has no description
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Oligocene Biomarker Temperature Estimates from ODP Hole 154-929A
This dataset has no description
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Middle Miocene census counts of Coccolithus and Reticulofenestra morphospecie...
This dataset has no description
