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Geochemical provenance analysis of fine-grained sediment of sediment core AND1-1
Bulk chemical fine-grained sediment compositions from southern Victoria Land glacimarine sediments provide significant constraints on the reconstruction of sediment provenance... -
Petrology and geochemistry of the AND-1B Core
Petrologic descriptions will follow a division related to both grain size and lithology like that adopted in Cape Roberts investigation (Cape Roberts Science Team 2000,... -
Porosity and density of the AND-1B sediment core
A study of density and porosity is presented for the 1285-m-long AND-1B core recovered from a flexural moat in the McMurdo Sound (Antarctica) in order to interpret sediment... -
Physical properties and abundance of diatoms of the ANDRILL AND1-1B drill core
In the austral summer of 2006/7 the ANDRILL MIS (ANtarctic geological DRILLing- McMurdo Ice Shelf) project recovered a 1285 m sediment core from beneath the Ross Ice Shelf near... -
Documentation of the ANDRILL AND1-1B drill cores from below McMurdo Ice Shelf
This data collection represents core descriptions of ANDRILL AND1-1B drill core. -
Relative abundance of diatom species in the ANDRILL AND1-1B drill core, 363.7...
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Age-Depth tie points for drill core ANDRILL 1B
Antarctica New Zealand Sir Robin Irvine PhD Scholarship awarded to B.D. Scientific Committee of Antarctic Research Fellowship awarded to B.D. New Zealand Ministry of Business... -
(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... -
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... -
(Table 1) Visual estimates of mineral and matrix percentages from AND1-1B thi...
In the original table, #0 is given as T. It is assumed here, that T means traces. However, the T is not explained in the article. -
(Table S4) Rock magnetic parameters measured on the ANDRILL AND1-1B drill core
Empty cells denotes an indeterminate analysis -
(Table S1) Diatom abundance according to ice cycles in ANDRILL AND1-1B drill ...
The influence of Antarctica and the Southern Ocean on Late Pliocene global climate reconstructions has remained ambiguous due to a lack of well-dated Antarctic-proximal,... -
Age model of the ANDRILL AND1-1B drill core, 382.38 to 459.19 m
Age model developed for samples analyzed in: Monien, Donata and Kuhn, Gerhard (2008, doi:10.1594/PANGAEA.708148) -
Physical properties of the ANDRILL AND1-1B drill core, 382.26 to 459.76 m
Wet bulk density and porosity data taken from: Niessen, F., D. Magens, and A. C. Gebhardt (2007, hdl:10013/epic.30000.d001). See doi:10.1594/PANGAEA.676905 for data. Dry bulk... -
(Table S3) Fe-oxide compositions from energy dispersive x-ray analysis of the...
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Core description of the ANDRILL AND1-1B drill core (resolution: 100 m)
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Core description of the ANDRILL AND1-1B drill core (resolution: 1 m)
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Core description of the ANDRILL AND1-1B drill core (resolution: 4 m)
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Core description of the ANDRILL AND1-1B drill core (overview)
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Interpretation of the depositional environments from the ANDRILL AND1-1B dril...
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