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Organic carbon accumulation, LGM
LGM (Last Glacial Maximum), average value of core section between 19 and 23 kyr BP or nearest sampled core depth -
Organic carbon accumulation, Holocene
Holocene, average value of core section between 4 and 8 kyr BP or nearest sampled core depth -
(Table 2c) Stable isotope ratios of Globigerinoides sacculifer from sediment ...
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(Appendix 2) Compilation of mass accumulation rates from deep sea sediments d...
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(Table 1) Foraminifera weight, size index and CO3 concentrations of core top ...
Down water column traverses of core top weights for three planktonic species confirm Lohmann's (1995) relationship between foraminifera shell weight loss and bottom water... -
Global data compilation of benthic data sets II
In this study we present a global distribution pattern and budget of the minimum flux of particulate organic carbon to the sea floor (J POC alpha). The estimations are based on... -
Radionuclides and accumulation rates of sediments from the equatorial Atlantic
Variations in carbonate flux and dissolution, which occurred in the equatorial Atlantic during the last 24,000 years, have been estimated by a new approach that allows the... -
Comparison between radiocarbon ages obtained on coexisting planktonic foramin...
As a test of the reliability of paleocean ventilation rates reconstructed from radiocarbon age differences between planktonic and benthic foraminifera, measurements have been... -
Stable carbon and oxygen isotope ratios of benthic foraminifera
Carbon isotopic measurements on the benthic foraminiferal genus Cibicidoides document that mean deep ocean delta13C values were 0.46 per mil lower during the last glacial... -
Stable carbon and oxygen isotope ratios of planktonic foraminifera from the e...
Carbon isotopic records of nutrient-depleted surface water place constraints on the past fertility of the oceans and on past atmospheric pCO2 levels. The best records of... -
Size-related stable isotope changes in Late Cretaceous and Recent planktic fo...
The paleoecology of Cretaceous planktic foraminifera during the Late Cenomanian to Coniacian period (~95-86 Ma) remains controversial since much of the tropical marine record is... -
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Pre-industrial Holocene (pi-HOL) paleo-dust record
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Global marine radiocarbon data compilation for the last deglaciation, spline ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, global ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, zonal a...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
(Table 1) Shell mass and chemistry of Globigerinoides sacculifer
Using bathymetric transects of surface sediments underlying similar sea surface temperatures but exposed to increasing dissolution, we examined the processes which affect the... -
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle... -
Trace element to calcium ratios and hydrological data for Trilobatus sacculif...
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Trace element to calcium ratios and hydrological data for Globigerinoides rub...
This dataset has no description