Methane excess in Arctic surface water-triggered by sea ice formation and melting
about
Methylphosphonate metabolism by Pseudomonas sp. populations contributes to the methane oversaturation paradox in an oxic freshwater lake.The Transpolar Drift conveys methane from the Siberian Shelf to the central Arctic Ocean.Carbon cycling fed by methane seepage at the shallow Cumberland Bay, South Georgia, sub-AntarcticSpatial distribution of dissolved methane and its source in the western Arctic OceanMethane fluxes from the sea to the atmosphere across the Siberian shelf seas
P2860
Methane excess in Arctic surface water-triggered by sea ice formation and melting
description
2015 nî lūn-bûn
@nan
2015 թուականի Նոյեմբերին հրատարակուած գիտական յօդուած
@hyw
2015 թվականի նոյեմբերին հրատարակված գիտական հոդված
@hy
2015年の論文
@ja
2015年論文
@yue
2015年論文
@zh-hant
2015年論文
@zh-hk
2015年論文
@zh-mo
2015年論文
@zh-tw
2015年论文
@wuu
name
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@ast
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@en
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@nl
type
label
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@ast
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@en
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@nl
prefLabel
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@ast
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@en
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@nl
P2093
P2860
P356
P1433
P1476
Methane excess in Arctic surface water-triggered by sea ice formation and melting
@en
P2093
P2860
P2888
P356
10.1038/SREP16179
P407
P50
P577
2015-11-10T00:00:00Z
P5875
P6179
1027617671