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4.5. Natural remanent magnetization of SLW1 sediment cores
Results from the NRM step, which is the very first measurement for all samples, without any prior magnetic treatment (i.e., the 0 mT demagnetization step). -
4.4. Documentation of sediment core SLW1_PC1
High-resolution line-scan imagery of the split core. High-resolution core radiographs of the split cores were taken using a Torrex 120-D radiograph at Antarctic Marine Geology... -
4.4. Documentation of sediment core SLW1_SLW_MC1A
High-resolution line-scan imagery of the split core. High-resolution core radiographs of the split cores were taken using a Torrex 120-D radiograph at Antarctic Marine Geology... -
4.4. Documentation of sediment core SLW1_PEC1
High-resolution line-scan imagery of the split core. High-resolution core radiographs of the split cores were taken using a Torrex 120-D radiograph at Antarctic Marine Geology... -
4.4. Documentation of sediment core SLW1_SLW_MC3A
High-resolution line-scan imagery of the split core. High-resolution core radiographs of the split cores were taken using a Torrex 120-D radiograph at Antarctic Marine Geology... -
Investigation of Quaternary diatoms in sediment core CRP-1 from the Ross Sea,...
In the first season of drilling, the Cape Roberts Project (CRP) recovered one drillcore (CRP-l) from Roberts Ridge in western McMurdo Sound, Ross Sea, Antarctica Diatom... -
Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antar...
Marine diatoms are the primary biostratigraphical and paleoenvironmental tool for interpreting the upper Palaeogene and lower Neogene strata recovered during the second drilling... -
Core scans and lithologic analysis of Subglacial Lake Whillans sediment cores
The hydrologic system beneath the Antarctic Ice Sheet is thought to influence both the dynamics and distribution of fast flowing ice streams, which discharge most of the ice... -
Age model of sediment core CRP-1
This dataset has no description
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(Table S1) Chronostratigraphic constrains for sediment core AND1-1B
Thirty years after oxygen isotope records from microfossils deposited in ocean sediments confirmed the hypothesis that variations in the Earth's orbital geometry control the ice...
