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Distribution of phytolithes in CRP sediment cores from the Ross Sea, Antarctica
Phytoliths (siliceous plant microfossils) have been recovered from Cenozoic sediments (c. 34 to 17 Ma) in the CRP-2/2A and CRP-3 drillholes cored off Cape Roberts, Victoria Land... -
Investigations on volcanic rocks in sediment core CRP-3 from the Ross Sea, An...
The petrography, mineralogy and geochemistry of volcanic and subvolcanic rocks in CRP-3 core have been examined in detail in order to characterise and to compare them with... -
Stable isotope ratios measured on molluscan from the CRP sediment cores in th...
Stable isotope analyses of marine bivalve growth increment samples have been used to estimate early Oligocene (29.4 - 31.2) Ma and early Miocene (24.0 Ma) seafloor... -
Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica
An 823 m thick glaciomarine Cenozoic section sitting unconformably on the Lower Devonian Beacon Supergroup was recovered in CRP-3. This paper reviews the chronostratigraphical... -
Sand geochemistry on sediment core CRP-3 from the Ross Sea, Antarctica
A total of 167 samples distubuted throughout the CRP-3 drillhole from 5.77 to 787.68 mbsf and representing fine to coarse sandstones have been analysed by X-ray fluorescence... -
Geochemistry of basement clasts from sediment core CRP-3 in the ross Sea, Ant...
Distribution patterns and petrographical and mineral chemistry data are described for the most representative basement lithologies occuring as clast in the c. 824 m thick... -
Geochemistry of minerals in CRP sediment cores from the Ross Sea, Antarctica
Sixty-four volcanic chists, sandstones and tephras between 5.95 and 618.19 meters below sea floor (mbsf) in the Cape Roberts Project cores 2 and 2A cores (CRP-2/2A) were... -
Abundance of ostracoda in sediment cores CRP-1 and CRP-2
Sparse, poorly preserved late Oligocene (3 species) and early Miocene (4 species) ostracod faunas have been recovered from CRP-2A, while relatively more abundant Quaternary... -
Clay mineralogy of Cape Roberts sediment cores
The clay mineral assemblages of the ca. 1600 m thick Cenozoic sedimentary succession recovered at the CRP-1, CRP-2/2A and CRP-3 drill sites off Cape Roberts on the McMurdo Sound... -
Diatom abundances in sediment core CESAR_83-006
The modern Arctic Ocean is regarded as a barometer of global change and amplifier of global warming (Graversen et al., 2008, doi:10.1038/nature06502) and therefore records of... -
Semiquantitative occurence of various minerals in sediment core CRP-2A
The mineralogy of the lower Oligocene to Quaternary sediments of core CRP-2/2A drilled on the continental shelf of McMurdo Sound in Ross Sea, Antarctica, was examined by the... -
Clay and smectite analysis of sediment core CRP-2A
Sediments of the CRP-2/2A drill core from the continental shelf of McMurdo Sound in Ross Sea, Pacific sector of the Southern Ocean, have been investigated for their clay mineral... -
Core derived downhole logs for holes CRP-2 and CRP-2A
In the northern McMurdo Sound (Ross Sea, Antarctica), the CRP-2/2A drillhole targeted the western margin of the Victoria Land Basin to investigate Neogene to Palaeogene climatic... -
Smoothed abundance of bulk mineralogy in the Cenozoic sediments of core CRP-3
The mineralogy of the lower Oligocene (to possibly upper Eocene) sediments of core CRP-3 drilled on the continental shelf of McMurdo Sound in the Ross Sea, Antarctica, has been... -
Clay and smectite content in sediment core CRP-3
The Cenozoic sediments of the CRP-3 drill core from the continental shelf of McMurdo Sound in Ross Sea, Pacific sector of the Southern Ocean, have been investigated for their... -
Temperature and resistivity profile of drill hole CRP-2A
In the northern part of McMurdo Sound (Ross Sea, Antarctica), drillhole CRP-2/2A targeted he western margin of the Victoria Land basin to investigate Neogene to Palaeogene... -
Carbon and nitrogen of sediment core CRP-2A (Table 1)
Sediments and rocks recovered in CRP-2/2A coring operations contain relatively little organic matter (average TOC=0.28%) and very small amounts of solvent-soluble organic... -
Geochemistry on smectites in sediment cores CRP-1 and CRP-2 from the Ross Sea...
TEM (transmission electron microscopy) observations and microanalyses on smectite microparticles in the sediments of the CRP-2A core were carried out to determine their origin... -
Grain size distribution and parameter in surface sediment samples from Alpha ...
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Distribution of the main heavy minerals identified in sediment core CRP-2/2A
Heavy minerals from the lower Oligocene to Quaternary sediments of the CRP-2/2A drill core have been analysed in order to characterize the mineralogical composition of the...