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Table 9: Astrochronology for ODP Site 208-1264
This dataset has no description
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Table 8: Correlation ties between ODP Site 208-1264 and Site 208-1265
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Table 4: Splice tie table ODP Site 208-1264
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Table 3: Revised offsets of ODP Hole 208-1264C
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Table 2: Revised offsets of ODP Hole 208-1264B
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Table 1: Revised offsets of ODP Hole 208-1264A
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Table 7: Mapping pairs of ODP Hole 208-1264C
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Table 6: Mapping pairs of ODP Hole 208-1264B
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Table 5: Mapping pairs of ODP Hole 208-1264A
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Climate, cryosphere and carbon cycle controls on Southeast Atlantic orbital-s...
These are the supplementary datasets for the manuscript: Drury, A.J., Liebrand, D., Westerhold, T., Beddow, H., Hodell, D., Rohlfs, N., Wilkens, R.H., Lourens, L., 'History of... -
Abyssal warming trend in the Vema Chanel, South Atlantic
Temperature time series sampled by instruments moored near the bottom in the Vema Channel, South Atlantic. -
Benthic foraminifera stable isotope records from shallow depths of western So...
Here we present oxygen and carbon isotope records of benthic foraminifera species from the continental shelf sediments influenced by upwelling events in the southwestern... -
Environmental controls on the Emiliania huxleyi calcite mass, supplement to: ...
Although ocean acidification is expected to impact (bio)calcification by decreasing the seawater carbonate ion concentration, [CO3]2-, there exists evidence of non-uniform... -
The effects of hypercapnia on the West Coast rock lobster (Jasus lalandii) th...
The cold water palinurid Jasus lalandii ('West Coast rock lobster') is a commercially important crustacean in South Africa and Namibia and inhabits the Benguela Current Eastern... -
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM...
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) from u-channel samples from Core MD07-3077. The RPI proxies were determined from stepwise alternating... -
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM...
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) for u-channel samples from Core MD07-3076. The RPI proxies were determined from stepwise alternating... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Laschamp excursion from discrete (2x2 cm²) samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Laschamp excursion from u-channel samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Iceland Basin excursion from u-channel samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Iceland Basin excursion from discrete (2x2 cm²) samples from...