Sökning: WFRF:(Dillon John) > Lakes and reservoir...
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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