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Record #213306:

Spatial variability of CO₂ emissions from newly exposed paraglacial soils at a glacier retreat zone on King George Island, Maritime Antarctica / André Thomazini, and 5 others.

Title: Spatial variability of CO₂ emissions from newly exposed paraglacial soils at a glacier retreat zone on King George Island, Maritime Antarctica / André Thomazini, and 5 others.
Author(s): Thomazini, André.
Date: 2014.
In: Permafrost and Periglacial Processes. (2014.), Vol. 25(4) (2014)
Abstract: Reports on spatial zoning of CO₂ emissions from soil and vegetation along transect in front of retreating margin of Ecology Glacier in Admiralty Bay, King George Island, South Shetlands, near Polish Antarctic station Henryk Arctowski, with aim of identifying potential contribution to atmospheric CO₂ as climate change occurs. Identifies soil formation and vegetation following deglaciation as key drivers of CO₂ emissions.
Notes:

Permafrost and Periglacial Processes. Vol. 25(4) :233-242 (2014).

Keywords: 551.324 -- Land ice.
551.324.22 -- Glaciers: Ecology.
551.324.6 -- Land ice, fluctuation.
574 -- Ecology.
574.4 -- Ecology, terrestrial.
631.4 -- Soil science.
551.58 -- Climatology.
551.583 -- Climatic changes.
551.588.5 -- Climate, relationship with ice.
546.264-31 -- Carbon dioxide.
E9 -- Glaciology: meteorology and climatology.
(*7) -- Antarctic regions.
(*726) -- Maritime Antarctic.
(*726.1) -- South Shetland Islands.
(*726.14) -- King George Island group.
SPRI record no.: 213306

MARCXML

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100 1# ‡aThomazini, André.
245 10 ‡aSpatial variability of CO₂ emissions from newly exposed paraglacial soils at a glacier retreat zone on King George Island, Maritime Antarctica /‡cAndré Thomazini, and 5 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2014.
300 ## ‡ap. 233-242 :‡bill., diags., tables, maps.
500 ## ‡aPermafrost and Periglacial Processes. Vol. 25(4) :233-242 (2014).
520 3# ‡aReports on spatial zoning of CO₂ emissions from soil and vegetation along transect in front of retreating margin of Ecology Glacier in Admiralty Bay, King George Island, South Shetlands, near Polish Antarctic station Henryk Arctowski, with aim of identifying potential contribution to atmospheric CO₂ as climate change occurs. Identifies soil formation and vegetation following deglaciation as key drivers of CO₂ emissions.
530 ## ‡aAlso issued online ‡uurn:doi:10.1002/ppp.1818‡uhttps://dx.doi.org/10.1002/ppp.1818
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers: Ecology.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡a574.4 -- Ecology, terrestrial.‡2udc
650 07 ‡a631.4 -- Soil science.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a546.264-31 -- Carbon dioxide.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*726) -- Maritime Antarctic.‡2udc
651 #7 ‡a(*726.1) -- South Shetland Islands.‡2udc
651 #7 ‡a(*726.14) -- King George Island group.‡2udc
773 0# ‡7nnas ‡tPermafrost and Periglacial Processes. ‡gVol. 25(4) (2014) ‡wSPRI-102743
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