Global Change Master Directorygsfc-gcmduso@mail.nasa.gov502013-05-18T11:03:15Zamd Search: [Parameters: Topic='OCEANS', Term='MARINE SEDIMENTS', Variable_Level_1='TERRIGENOUS SEDIMENTS']http://mddemo.gsfc.nasa.gov/KeywordSearch/OpenSearch.do 19 0 http://gcmd.gsfc.nasa.gov/getdif.htm?[AADC]ASAC_1220Antarctic ice sheet history and stability: baseline palaeoclimate research on the Pagodroma Group, Prince Charles Mountains.68.1093,-70.5401,68.1093,-70.540168.1058,-70.7089,68.1058,-70.708968.1007,-70.7128,68.1007,-70.712868.098,-70.7146,68.098,-70.71462000-11-01T00:00:00Z2000-12-20T00:00:00Z2011-05-10T04:00:00ZDetailed sedimentary information and palaeontological samples were collected from Battye Glacier Formation, of the Pagodroma Group in the Prince Charles Mountains, an area where little information ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NSF-ANT05-38580Antarctica's Geological History Reflected in Sedimentary Radiogenic Isotopes60.0,-70.0,180.0,-60.02006-09-15T00:00:00Z2010-08-31T00:00:00Z2010-11-23T05:00:00ZThis project studies sediment from the ocean floor to understand Antarctica's geologic history. Glacially eroded from the Antarctic continent, these sediments may offer insight into the 99% Antarctica ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NSF-ANT08-38842Determining Middle Miocene through Pliocene Changes in Paleo Ice-flow and Basal Ice Conditions in East Antarctica through Sedimentological Analyses of Core Samples160.0,-78.0,-150.0,-68.02009-07-01T00:00:00Z2010-06-30T00:00:00Z2010-09-07T04:00:00ZThis award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5). The project aims on studying sediment cores collected from Prydz Bay and the Ross Sea to unravel the ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]ODP1095-1101-sedimentologySedimentology of Antarctic Peninsula drift deposits recovered at ODP Sites 1095 and 11012010-07-07T04:00:00ZData include the percent of terrigenous and opaline components, mass accumulation rates of each, grainsize of the terrigenous component, and magnetic fabric (anisotropy of magnetic susceptibility).http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]SB2006Antarctic Peninsula magnetic granulometry2010-07-02T04:00:00ZData consist of magnetic hysteresis parameters, Curie temperatures, Verwey
transition temperatures, isotropic points, and susceptibility for western
Antarctic Peninsula bed ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2006-017Black Sea/Red Sea Oxygen Isotope and Terrigeneous Flux Data 57.96,29.5,57.96,29.531.17,41.53,31.17,41.5331.07,41.44,31.07,41.442009-01-15T05:00:00ZThis data set consists of Black Sea/Red Sea Oxygen Isotope and Terrigeneous
Flux Data. High-resolution sediment cores from the southwestern Black Sea and
the northernmost Gulf of Aqaba ...http://gcmd.gsfc.nasa.gov/getdif.htm?[AADC]ASAC_1044Wilkes Land Glacial History (WEGA)142.0,-67.5,146.0,-64.02000-09-30T00:00:00Z2001-03-31T00:00:00Z2008-11-07T05:00:00ZA collaborative Italian/Australian marine geoscience research voyage to the George Vth Land sector of the East Antarctic continental margin was carried out between 11th February and 20th March, 2000, ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2004-068Sea of Okhotsk Paleoproductivity and Terrigenous Flux Data 149.96,53.95,149.96,53.95150.98,51.71,150.98,51.712007-03-08T05:00:00ZThe data set on cores MD01-2415 and LV28-42-4 from the central Sea of Okhotsk
(NW-Pacific) consists of a variety of proxy data reflecting changes in
paleoproductivity, terrigenous flux, and sea ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_98-002Eocene/Oligocene Boundary Paleoproductivity Data 59.76,86.86,59.76,86.86134.92,88.04,134.92,88.04144.38,87.53,144.38,87.539.59,86.23,9.59,86.23-14.0,85.33,-14.0,85.332007-03-01T05:00:00ZStable isotope and 14C dates for 5 cores in the central Arctic Ocean.
Stable Isotope Data Files (*.data.txt):
core depth, delta O-18 (Neogloboquadrina pachyderma sin.), delta ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2001-012Central Equatorial Pacific Export Production and CaCO3 Dissolution Data -140.0,-5.0,-140.0,4.02007-02-27T05:00:00ZThis data set contains Central Equatorial Pacific Export Production and CaCO3
Dissolution Data.
Inorganic chemical analysis of five JGOFS piston cores on a meridional transect
at ~140 West across ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2002-010Southern Ocean Elemental Data 5.12,-48.57,5.12,-48.57-4.93,-53.88,-4.93,-53.88106.52,-44.88,106.52,-44.882007-01-05T05:00:00ZLatimer and Filippelli (2001) Southern Ocean Elemental Data. Geochemistry
from several sites along the Polar Front in the Southern Ocean, indicating
significant changes in terrigenous elements ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_1999-038Western Tropical Atlantic Sedimentation Data -45.0,-15.0,-10.0,15.02006-12-04T05:00:00ZThis data set consists of Magnetic susceptibility, % reflectance, and first
derivatives of % reflectance for Ocean Drilling Program Sites 925-929
following the shipboard splice.
PLEASE NOTE: Files ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_1998-029Arabian Sea Sediment Trap Dust Flux and Grain Size Data 58.48,10.0,65.0,17.41994-10-01T00:00:00Z1995-12-31T00:00:00Z2006-11-16T05:00:00ZThis data set consists of lithogenic flux and grain size data from four
sediment trap moorings deployed perpendicularly to the coast of the Arabian
Peninsula (~200 to 1250 km offshore, ~1000 to ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2002-045DIRTMAP Version 2. Last Glacial Maximum, Late Holocene, and Modern Eolian Fluxes from Ice Cores, Marine Sediments, Marine Sediment Traps, and Terrestrial Deposits-180.0,-90.0,180.0,90.01980-01-01T00:00:00Z1996-12-31T00:00:00Z2006-08-31T04:00:00ZThe records of dust accumulation rates included here represent the second
version of the DIRTMAP data base, including dust information from ice cores,
marine sediments, marine sediment traps, and ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]Goldstein_OPP_0088054Establishing the pattern of Holocene-LGM changes in sediment contributions from Antarctica to the Southern Ocean-180.0,-73.54,180.0,-39.572005-12-21T05:00:00ZTerrigenous clastic sediments are brought to the ocean from continental sources
via rivers, ice and wind, and distributed within the ocean by surface and deep
currents. By investigating long-lived ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]MetalIonsInMarineAndLacustrEnvEvolution and biogeochemical cycles of metal species in marine and lacustrine environments162.55,-77.53,176.83,-71.931995-12-01T00:00:00Z2004-02-28T00:00:00Z2005-06-27T04:00:00Z1995/96
Characterization of minor and trace metals in lacustrine ecosystems (Carezza
Lake, Inexpressible Island, Tarn Flat, Edmondson Point). Determinations in
lake waters, sediments, algae and soil. ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO-2002-045DIRTMAP Version 2. Last Glacial Maximum, Late Holocene, and Modern Eolian Fluxes from Ice Cores, Marine Sediments, Marine Sediment Traps, and Terrestrial Deposits-180.0,-90.0,180.0,90.02005-05-18T04:00:00ZThe records of dust accumulation rates from version 2 (2002) and 1 (2001) of
the DIRTMAP data base, including dust information from ice cores, marine
sediments, marine sediment traps, and loess sediments. ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2003-023Grain Size and Magnetic Fabric Data-127.38,39.27,-127.38,39.27-127.18,39.59,-127.18,39.59-74.83,31.25,-74.83,31.25-125.67,42.08,-125.67,42.082004-03-22T05:00:00ZGrain Size and Magnetic Fabric Data interpreted in terms of
depositional environment and paleocurrent strength.
ABSTRACT (from the online documentation):
The combined use of grain size and magnetic ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NL_ANTARCTICA_ICESHEET_EXTENTExtent of the grounded Antarctic ice sheet in space and time-71.0,-69.0,-67.0,-68.0-106.0,-75.0,100.0,-71.0163.0,-78.0,167.0,-74.01996-04-01T00:00:00Z1998-04-01T00:00:00Z2001-06-26T04:00:00ZLimited exposure is a major drawback when using drillcores for
reconstructing past glacial environments: direct observations of
sediments are restricted to the width of the cores and only provide ...