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100			_a20170904a2009 k y0engy50 ba
101	0		_aeng
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181		0	_ai
182		0	_ab
200	1		_aOut-gassing of CO[2] from Siberian Shelf seas by terrestrial organic matter decomposition _fL. G. Anderson [et al.]
203			_aText _celectronic
300			_aTitle screen
320			_a[References: 34 tit.]
330			_aThe Siberian shelf seas cover large shallow areas that receive substantial amounts of river discharge. The river runoff contributes nutrients that promote marine primary production, but also dissolved and particulate organic matter. The coastal regions are built up of organic matter in permafrost that thaws and result in coastal erosion and addition of organic matter to the sea. Hence there are multiple sources of organic matter that through microbial decomposition result in high partial pressures of CO2 in the shelf seas. By evaluating data collected from the Laptev and East Siberian Seas in the summer of 2008 we compute an excess of DIC equal to 10 · 1012 g C that is expected to be outgassed to the atmosphere and suggest that this excess mainly is caused by terrestrial organic matter decomposition.
333			_aРежим доступа: по договору с организацией-держателем ресурса
461			_tGeophysical Research Letters
463			_tVol. 36, iss. 20 _v[P. L20601/1-L20601/6] _d2009
610	1		_aэлектронный ресурс
610	1		_aтруды учёных ТПУ
610	1		_aрастворенные газы
610	1		_aдвуокись углерода
610	1		_aдегазация
610	1		_aСеверный Ледовитый океан
610	1		_aобзоры
701		1	_aAnderson _bL. G.
701		1	_aJutterström _bS.
701		1	_aHjalmarsson _bS.
701		1	_aWålström _bI.
701		1	_aSemiletov _bI. P. _cgeographer _cProfessor of Tomsk Polytechnic University, doctor of geographical Sciences _f1955- _gIgor Petrovich _2stltpush _3(RuTPU)RU\TPU\pers\34220
801		2	_aRU _b63413507 _c20180220 _gRCR
856	4		_uhttp://dx.doi.org/10.1029/2009GL040046
942			_cCF