Lakes and reservoirs as regulators of carbon cycling and climate

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Fältnamn	Indikatorer	Metadata
000		04221naa a2200685 4500
001		oai:DiVA.org:uu-142160
003		SwePub
008		110113s2009 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-1421602 URI
024	7	a https://doi.org/10.4319/lo.2009.54.6_part_2.22982 DOI
040		a (SwePub)uu
041		a engb eng
042		9 SwePub
072	7	a ref2 swepub-contenttype
072	7	a for2 swepub-publicationtype
100	1	a Tranvik, Lars J.u Uppsala universitet,Institutionen för ekologi och evolution,Limnologi4 aut0 (Swepub:uu)larstran
245	1 0	a Lakes and reservoirs as regulators of carbon cycling and climate
264		c 2009-11-16
264	1	b Wiley,c 2009
338		a print2 rdacarrier
520		a We explore the role of lakes in carbon cycling and global climate, examine the mechanisms influencing carbon pools and transformations in lakes, and discuss how the metabolism of carbon in the inland waters is likely to change in response to climate. Furthermore, we project changes as global climate change in the abundance and spatial distribution of lakes in the biosphere, and we revise the estimate for the global extent of carbon transformation in inland waters. This synthesis demonstrates that the global annual emissions of carbon dioxide from inland waters to the atmosphere are similar in magnitude to the carbon dioxide uptake by the oceans and that the global burial of organic carbon in inland water sediments exceeds organic carbon sequestration on the ocean floor. The role of inland waters in global carbon cycling and climate forcing may be changed by human activities, including construction of impoundments, which accumulate large amounts of carbon in sediments and emit large amounts of methane to the atmosphere. Methane emissions are also expected from lakes on melting permafrost. The synthesis presented here indicates that (1) inland waters constitute a significant component of the global carbon cycle, (2) their contribution to this cycle has significantly changed as a result of human activities, and (3) they will continue to change in response to future climate change causing decreased as well as increased abundance of lakes as well as increases in the number of aquatic impoundments.
650	7	a NATURVETENSKAPx Biologi0 (SwePub)1062 hsv//swe
650	7	a NATURAL SCIENCESx Biological Sciences0 (SwePub)1062 hsv//eng
653		a Biology
653		a Biologi
700	1	a Downing, John A.4 aut
700	1	a Cotner, James B.4 aut
700	1	a Loiselle, Steven A.4 aut
700	1	a Striegl, Robert G.4 aut
700	1	a Ballatore, Thomas J.4 aut
700	1	a Dillon, Peter4 aut
700	1	a Finlay, Kerri4 aut
700	1	a Fortino, Kenneth4 aut
700	1	a Knoll, Lesley B.4 aut
700	1	a Kortelainen, Pirkko L.4 aut
700	1	a Kutser, Tiit4 aut
700	1	a Larsen, Soren4 aut
700	1	a Laurion, Isabelle4 aut
700	1	a Leech, Dina M.4 aut
700	1	a McCallister, S. Leigh4 aut
700	1	a McKnight, Diane M.4 aut
700	1	a Melack, John M.4 aut
700	1	a Overholt, Erin4 aut
700	1	a Porter, Jason A.4 aut
700	1	a Prairie, Yves4 aut
700	1	a Renwick, William H.4 aut
700	1	a Roland, Fabio4 aut
700	1	a Sherman, Bradford S.4 aut
700	1	a Schindler, David W.4 aut
700	1	a Sobek, Sebastian4 aut
700	1	a Tremblay, Alain4 aut
700	1	a Vanni, Michael J.4 aut
700	1	a Verschoor, Antonie M.4 aut
700	1	a von Wachenfeldt, Eddieu Uppsala universitet,Institutionen för ekologi och evolution4 aut
700	1	a Weyhenmeyer, Gesa A.u Uppsala universitet,Institutionen för ekologi och evolution,Limnologi4 aut0 (Swepub:uu)gesaweyh
710	2	a Uppsala universitetb Institutionen för ekologi och evolution4 org
773	0	t Limnology and Oceanographyd : Wileyg 54:6:2, s. 2298-2314q 54:6:2<2298-2314x 0024-3590x 1939-5590
856	4	u https://aslopubs.onlinelibrary.wiley.com/doi/pdfdirect/10.4319/lo.2009.54.6_part_2.2298
856	4 8	u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-142160
856	4 8	u https://doi.org/10.4319/lo.2009.54.6_part_2.2298

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