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Distribution of planktic foraminifera at the last glacial maximum
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(Table 2) Age determination on sediment core CH82-20
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Radiocarbon age determinations on sediment core CH82-24
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Planktic foraminifera counts of sediment core CHN82-24
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(Table 1) Stable isotope ratios of foraminifera in sediment core CH82-20
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Table 1. Comparison of samples cleaned by old and new methods for various cores
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(Table 2) Age model of sediment core CHN82-24
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Age determination, foraminiferal abundance and stable isotope ratios of sedim...
A core from the Mid-Atlantic Ridge at 43.5°N and ~3 km water depth shows distinct evidence of the deglacial events known as Heinrich event 1 (probably the marine equivalent of... -
Stable isotope analysis on sediment core CHN82-24
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Age models and stable isotope record of sediment cores from the Atlantic Ocean
The high-resolution delta18O and delta13C records of benthic foraminifera from a 150,000-year long core from the Caribbean Sea indicate that there was generally high delta13C... -
Stable isotope and Cd/Ca ratios of Neogloboquadrina pachyderma in high-latitu...
Recent studies have stressed the role of high latitude nutrient levels and productivity in controlling the carbon isotopic composition of the deep sea and the CO2 content of the... -
(Table IV) Stable carbon and oxygen isotope ratios and temperature estimates ...
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Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
Summary of sediment core sites of water regions in the Atlantic and Pacific o...
Summary of sediment core sites including number of available data for each of the five proxies used. Data columns indicate the site name, longitude (lon, °E), latitude (lat,... -
Age control of sediment core CHN82-24
GLAMAP and EPILOG differ because of low -resolution SST data -
Sea surface temperatures reconstructed from sediment core CHN82-24
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(Table 2) Trace metal ratios of various benthic foraminifera shells
Benthic foraminiferal d13C and Cd/Ca studies suggest that deep Atlantic circulation during the Last Glacial Maximum was very different from today, with high-nutrient (low d13C,... -
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... -
(Appendix 1) Stable carbon and oxygen isotope ratios of Cibicidoides spp. fro...
C. wuellerstorfi and C. kullenbergi -
Atlantic sea surface temperatures during the last glacial maximum (LGM) time ...
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