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Age-Depth tie points for drill core Cape Roberts 2/2A
Age tie points from 214.13 mbsf and above from: Acton et al. (2008). Age tie points from 214.14 to 1138.54 mbsf from Levy et al. (2016).Antarctica New Zealand Sir Robin Irvine... -
GDGT abundances and indices for Ross Sea sample sites
Note for AND1-1B (ANDRILL-1B): in samples with BIT values but no brGDGT values, the BIT has been taken from McKay et al. (2012).Antarctica New Zealand Sir Robin Irvine PhD... -
Glycerol dialkyl glycerol tetraether (GDGT) abundances, age-depth tie points ...
This data publication contains biostratigraphic age events for the CIROS-1 drill core, updated age ranges for a suite of samples from the McMurdo erratics sample collection,... -
Mean textural characters, size and ground attribution of volcanic clasts in s...
This dataset has no description
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Modal analyses of thin-sections of sediment core CRP-1 (Table 1)
During the course of the 1997 drilling campaign, lithostratigraphic boundaries were assigned to the CRP-l core on the basis of perceived changes in lithology. The geologically... -
(Table 1) Stable oxygen and carbon isotope composition of bivalve shells of s...
Bivalve shells from the CRP-l drillhole, Cape Roberts (Victoria Land Basin), have been analysed for their stable isotope composition to obtain information on Antarctic coastal... -
Physical properties of sediment core CRP-3
Drillhole CRP-3 in northern McMurdo Sound (Ross Sea, Antarctica) targeted the western margin of the Victoria Land basin to investigate Neogene to Palaeogene climate and tectonic... -
Physical properties of sediment core CRP-2A
In this paper the relationship between whole-core compressional wave velocities and gamma-ray attenuation porosities of sediments cored at CRP-2/2A is examined, and compared... -
Physical properties of sediment core CRP-1
The relationship between whole-core compressional wave velocities and gamma-ray attenuation porosities of sediments cored at CRP-1 is examined and compared with results from... -
Preliminiary results and documentation of sediment core CRP-3 from the Ross S...
The site for CRP-3, 12 km east of Cape Roberts (77.006°S; 103.719°E)was selecte to overlap the lower Oligocene strata cored in nearby CRP-2/2A, and to sample the oldest strata... -
(Table 1) Facies characteristics and their interpretations of sediment core C...
This dataset has no description
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(Table 2) Percentages of lithofacies through sediment cores CRP-2/2A devided ...
Depth = basal depth (mbsf). Note that the Pleistocene and Pliocene epochs are not well represented in the core in terms of thickness recovery, and thus reliability of the data... -
(Table 1) Facies characteristics and their interpretations of sediment cores ...
Ordinal number = facies number -
(Table 2) Percentage of facies in each lithostratigraphic unit of sediment co...
This dataset has no description
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(Table 1) Major and trace elements of sediment core CRP-3
The CRP-3 core, drilled in western McMurdo Sound in October and November 1999, penetrated 823 m of lower Oligocene (to possibly upper Eocene) glacially influenced sediments. The... -
(Table 1) Description of grain size, cement, and matrix in sediment core CRP-...
The presence of authigenic smectite in the lower Oligocene sandstones of the Cape Roberts Project core CRP-3 from the Victoria Land Basin of Antarctica is confirmed by scanning... -
Description of lithofacies associations and their interpreted settings from s...
Cape Roberts Project drillcore 1 was obtained from Roberts Ridge, a sea-floor high located at 77°S, 16 km offshore from Cape Roberts in western McMurdo Sound, Antarctica. The... -
Element abundances, loss on ignition, total analyzed abundances, CIA values, ...
The CRP-2/2A core, drilled in western McMurdo Sound in October and November 1998, penetrated 624 m of Quaternary. Pliocene, lower Miocene, and Oligocene glacigenic sediments.... -
Geochemistry on sediment core CRP-1 (Table 1)
The CRP-1 core penetrated 148 m of Quaternary and lower Miocene glacigenic sediments. This material complements the Eocene trhough Miocene strata that was cored previously at... -
Ice rafted debris distribution in sediment core CRP-1
Lonestone abundances in CRP-1 were investigated using three methods: core examination at Cape Roberts Camp, analysis of digital core images and follow-up core examination. For...
