Difference between revisions of "ODP1098B.Shevenell.2011"
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( Dataset (L) )
(Deleted PropertyValue: Citation = The disintegration of ice shelves, reduced sea-ice and glacier extent, and shifting ecological zones observed around Antarctica (Cook et al., 2005; Stammerjohn et al., 2008) highlight the impact of recent atmospheric (Steig et al., 2009) and oceanic warming (Gille, 2002) on the cryosphere. Observations (Cook et al., 2005; Stammerjohn et al., 2008) and models (Pollard and DeConto, 2009) suggest that oceanic and atmospheric temperature variations at Antarctica's margins affect global cryosphere stability, ocean circulation, sea levels and carbon cycling. In particular, recent climate changes on the Antarctic Peninsula have been dramatic, yet the Holocene climate variability of this region is largely unknown, limiting our abil) |
(Added PropertyValue: Description (L) = Marine sediment core ODP1145 was collected from the Drake Passage -64° 51' 43", -64° 12' 29". Radiocarbon, d18O, CDGT, and TEX86 on DefaultSensor and Neogloboquadrina pachyderma were made on the archive and interpreted as temperature.) |
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Contributor (L)=Eugene_W_Domack| | Contributor (L)=Eugene_W_Domack| | ||
Contributor (L)=Ciarán_Kelly| | Contributor (L)=Ciarán_Kelly| | ||
| − | + | DatasetVersion (L)=0.0.0| | |
| + | Description (L)=Marine sediment core ODP1145 was collected from the Drake Passage -64° 51' 43", -64° 12' 29". Radiocarbon, d18O, CDGT, and TEX86 on DefaultSensor and Neogloboquadrina pachyderma were made on the archive and interpreted as temperature.| | ||
| + | HasDOI (L)=10.1594/PANGAEA.769707| | ||
IncludesChronData (L)=ODP1098B.Shevenell.2011.ChronData1| | IncludesChronData (L)=ODP1098B.Shevenell.2011.ChronData1| | ||
IncludesPaleoData (L)=ODP1098B.Shevenell.2011.PaleoData1| | IncludesPaleoData (L)=ODP1098B.Shevenell.2011.PaleoData1| | ||
