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  • 1
    Publication Date: 2023-10-28
    Keywords: Aluminium oxide; AND1-1B; AND-1B; ANDRILL; Antarctic Geological Drilling; Calcium oxide; Calculated; Chromium(III) oxide; D-ANDRILL; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Identification; Magnesium oxide; Magnetite; Manganese oxide; McMurdo Ice Shelf; McMurdo Station; MIS; Niobium (V) oxide; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Silicon dioxide; SPP1158; Sum; Texture; Titanium dioxide; Vanadium(III) oxide; X-ray radiography; Zinc oxide
    Type: Dataset
    Format: text/tab-separated-values, 2172 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-10-28
    Keywords: AND1-1B; AND-1B; ANDRILL; Antarctic Geological Drilling; Coercivity; Coercivity/coercivity of remanence ratio; Coercivity of remanence; D-ANDRILL; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Kappabridge, AGICO KLY-4; Magnetization; McMurdo Ice Shelf; McMurdo Station; MIS; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Remanent magnetization, intensity, per unit mass; Remanent magnetization/magnetization ratio; Rock type; Saturation isothermal remanent magnetization, normalized; SPP1158; S-ratio (hematite/magnetite); Susceptibility, specific, ferromagnetic; Susceptibility, specific, high-field mass-normalized; Susceptibility, specific, low-field mass-normalized
    Type: Dataset
    Format: text/tab-separated-values, 7715 data points
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Brachfeld, Stefanie A; Pinzon, Juliana; Darley, Jason; Sagnotti, Leonardo; Kuhn, Gerhard; Florindo, Fabio; Wilson, Gary S; Ohneiser, Christian; Monien, Donata; Joseph, Leah H (2013): Iron oxide tracers of ice sheet extent and sediment provenance in the ANDRILL AND-1B drill core, Ross Sea, Antarctica. Global and Planetary Change, 110(C), 420-433, https://doi.org/10.1016/j.gloplacha.2013.09.015
    Publication Date: 2023-12-12
    Description: The AND-1B drill core recovered a 13.57 million year Miocene through Pleistocene record from beneath the McMurdo Ice Shelf in Antarctica (77.9°S, 167.1°E). Varying sedimentary facies in the 1285 m core indicate glacial-interglacial cyclicity with the proximity of ice at the site ranging from grounding of ice in 917 m of water to ice free marine conditions. Broader interpretation of climatic conditions of the wider Ross Sea Embayment is deduced from provenance studies. Here we present an analysis of the iron oxide assemblages in the AND-1B core and interpret their variability with respect to wider paleoclimatic conditions. The core is naturally divided into an upper and lower succession by an expanded 170 m thick volcanic interval between 590 and 760 m. Above 590 m the Plio-Pleistocene glacial cycles are diatom rich and below 760 m late Miocene glacial cycles are terrigenous. Electron microscopy and rock magnetic parameters confirm the subdivision with biogenic silica diluting the terrigenous input (fine pseudo-single domain and stable single domain titanomagnetite from the McMurdo Volcanic Group with a variety of textures and compositions) above 590 m. Below 760 m, the Miocene section consists of coarse-grained ilmenite and multidomain magnetite derived from Transantarctic Mountain lithologies. This may reflect ice flow patterns and the absence of McMurdo Volcanic Group volcanic centers or indicate that volcanic centers had not yet grown to a significant size. The combined rock magnetic and electron microscopy signatures of magnetic minerals serve as provenance tracers in both ice proximal and distal sedimentary units, aiding in the study of ice sheet extent and dynamics, and the identification of ice rafted debris sources and dispersal patterns in the Ross Sea sector of Antarctica.
    Keywords: ANDRILL; Antarctic Geological Drilling; D-ANDRILL; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-12-12
    Keywords: Aluminium oxide; ANDRILL; Antarctic Geological Drilling; Bottom grab (Smith-McIntyre); Bryd Glacier; Calcium oxide; Calculated; Central Transantractic Mountains; Chromium(III) oxide; D-ANDRILL; Darwin Glacier; DEPTH, sediment/rock; Dry Valleys; Event label; HAND; Identification; Koettlitz Glacier; Latitude of event; Lithology/composition/facies; Location of event; Longitude of event; Magnesium oxide; Magnetite; Manganese oxide; McMurdo Sound; Nathaniel B. Palmer; NBP0702; NBP0702_SMG1; Niobium (V) oxide; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; PRR-10347; PRR-10405; PRR-12732; PRR-13075; PRR-15009; PRR-15023; PRR-15046; PRR-15058; PRR-15078; PRR-21020; PRR-21092; PRR-21107; PRR-24463; PRR-24668; PRR-26033; PRR-26551; PRR-26612; PRR-4621; PRR-4998; PRR-7363; PRR-7372; PRR-7376; PRR-7378; Rock type; Ross Island; Sampling by hand; Silicon dioxide; Skelton Glacier; SMG; Southern Transantarctic Mountains; SPP1158; Sum; Tent Island; Texture; Titanium dioxide; Vanadium(III) oxide; X-ray radiography; Zinc oxide
    Type: Dataset
    Format: text/tab-separated-values, 1655 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-12-12
    Keywords: ANDRILL; Antarctic Geological Drilling; Bottom grab (Smith-McIntyre); Bryd; Bryd Glacier; Central Transantractic Mountains; Coercivity of remanence; D-ANDRILL; Darwin Glacier; DEPTH, sediment/rock; Dry Valleys; Event label; HAND; Kappabridge, AGICO KLY-4; Koettlitz Glacier; Latitude of event; Lithology/composition/facies; Location of event; Longitude of event; Magnetization; McMurdo Sound; Mt. Morning; Mulock Glacier; Nathaniel B. Palmer; NBP0702; NBP0702_SMG1; Northern Victoria Land; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; PRR-10347; PRR-10405; PRR-10445; PRR-11896; PRR-12420; PRR-12546; PRR-12550; PRR-12569; PRR-12597; PRR-12732; PRR-12952; PRR-13075; PRR-13627; PRR-13779; PRR-13839; PRR-13841; PRR-14003; PRR-14448; PRR-14471; PRR-14932; PRR-15008; PRR-15009; PRR-15023; PRR-15046; PRR-15058; PRR-15076; PRR-15078; PRR-15084; PRR-15085; PRR-15099; PRR-15100; PRR-15241; PRR-15858; PRR-15924; PRR-15938; PRR-15945; PRR-16054; PRR-18900; PRR-21020; PRR-21028; PRR-21047; PRR-21082; PRR-21092; PRR-21101; PRR-21107; PRR-21161; PRR-22956; PRR-23379; PRR-23456; PRR-23523; PRR-23528; PRR-23802; PRR-24463; PRR-24668; PRR-24930; PRR-25920; PRR-26033; PRR-26237; PRR-26266; PRR-26535; PRR-26539; PRR-26551; PRR-26552; PRR-26612; PRR-2720; PRR-3872; PRR-4009; PRR-4053; PRR-4621; PRR-4998; PRR-5307; PRR-5385; PRR-5453; PRR-5535; PRR-5614; PRR-6200; PRR-6460; PRR-6485; PRR-6787; PRR-6792; PRR-7091; PRR-7363; PRR-7372; PRR-7376; PRR-7377; PRR-7378; Remanent magnetization, intensity, per unit mass; Remanent magnetization/magnetization ratio; Rock type; Ross Island; Sampling by hand; Skelton Glacier; SMG; Southern Transantarctic Mountains; Southern Victoria Land; SPP1158; S-ratio (hematite/magnetite); Susceptibility, specific, high-field mass-normalized; Susceptibility, specific, low-field mass-normalized; Tent Island
    Type: Dataset
    Format: text/tab-separated-values, 798 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2018-08-10
    Description: The AND-1B drill core recovered a 13.57 million year Miocene through Pleistocene record from beneath the McMurdo Ice Shelf in Antarctica (77.9°S, 167.1°E). Varying sedimentary facies in the 1285 m core indicate glacial–interglacial cyclicity with the proximity of ice at the site ranging from grounding of ice in 917 m of water to ice free marine conditions. Broader interpretation of climatic conditions of the wider Ross Sea Embayment is deduced from provenance studies. Here we present an analysis of the iron oxide assemblages in the AND-1B core and interpret their variability with respect to wider paleoclimatic conditions. The core is naturally divided into an upper and lower succession by an expanded 170 m thick volcanic interval between 590 and 760 m. Above 590 m the Plio-Pleistocene glacial cycles are diatom rich and below 760 m late Miocene glacial cycles are terrigenous. Electron microscopy and rock magnetic parameters confirm the subdivision with biogenic silica diluting the terrigenous input (fine pseudo-single domain and stable single domain titanomagnetite from the McMurdo Volcanic Group with a variety of textures and compositions) above 590 m. Below 760 m, the Miocene section consists of coarse-grained ilmenite and multidomain magnetite derived from Transantarctic Mountain lithologies. This may reflect ice flow patterns and the absence of McMurdo Volcanic Group volcanic centers or indicate that volcanic centers had not yet grown to a significant size. The combined rock magnetic and electron microscopy signatures of magnetic minerals serve as provenance tracers in both ice proximal and distal sedimentary units, aiding in the study of ice sheet extent and dynamics, and the identification of ice rafted debris sources and dispersal patterns in the Ross Sea sector of Antarctica.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Location Call Number Limitation Availability
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