Magnitude and significance of carbon burial in lakes, reservoirs, and peatlands

Globally, lakes are currently accumulating organic carbon (OC) at an estimated annual rate of about 42 Tgṁyr −1 . Most of the OC in all but the most oligotrophic of these lakes is autochthonous, produced by primary production in the lakes. The sediments of reservoirs accumulate an additional 160 Tg annually, and peatlands contribute 96 Tg annually. These three carbon pools collectively cover less than 2% of the Earth9s surface and constitute a carbon sink of about 300 Tgṁyr −1 . Although the oceans cover 71% of the Earth9s surface, they accumulate OC at a rate of only about 100 Tgṁyr −1 .

[1]  J. Elwood,et al.  The role of lake and reservoir sediments as sinks in the perturbed global carbon cycle , 1982 .

[2]  Eric S. Menges,et al.  Patterns of Change in the Carbon Balance of Organic Soil-Wetlands of the Temperate Zone , 1986 .

[3]  P. Dillon,et al.  Photolytic regulation of dissolved organic carbon in northern lakes , 1997 .

[4]  S. Colman,et al.  Two episodes of meltwater influx from glacial Lake Agassiz into the Lake Michigan basin and their climatic contrasts , 1994 .

[5]  S. Colman,et al.  Holocene paleoclimatic evidence and sedimentation rates from a core in southwestern Lake Michigan , 1990 .

[6]  E. Gorham Northern Peatlands: Role in the Carbon Cycle and Probable Responses to Climatic Warming. , 1991, Ecological applications : a publication of the Ecological Society of America.

[7]  R. Bourbonniere,et al.  Southern Lake Michigan Sediments: Changes in Accumulation Rate, Mineralogy, and Organic Content , 1980 .

[8]  J. Ritchie Carbon content of sediments of small reservoirs , 1989 .

[9]  F. Mackereth Some chemical observations on post-glacial lake sediments , 1966, Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences.

[10]  James V. Gardner,et al.  Biogenic sedimentation beneath the California Current System for the past 30 kyr and its paleoceanographic significance , 1997 .

[11]  P. Meyers,et al.  Lacustrine organic geochemistry—an overview of indicators of organic matter sources and diagenesis in lake sediments , 1993 .

[12]  W. Dean Physical properties, mineralogy, and geochemistry of Holocene varved sediments from Elk Lake, Minnesota , 1993 .

[13]  E. Gorham,et al.  Fossil pigments in Minnesota lake sediments and their bearing upon the balance between terrestrial and aquatic inputs to sedimentary organic matter , 1975 .

[14]  J. Hedges,et al.  Processes controlling the organic carbon content of open ocean sediments , 1988 .

[15]  M. Stainton,et al.  Chemistry of Surface Sediments of Sixteen Lakes in the Experimental Lakes Area, Northwestern Ontario , 1971 .

[16]  P. Dillon,et al.  Storage of terrestrial carbon in boreal lake sediments and evasion to the atmosphere , 1996 .

[17]  G. Likens Primary Production of Inland Aquatic Ecosystems , 1975 .

[18]  E. Gorham,et al.  The diversity of pigments in lake sediments and its ecological significance , 1970 .

[19]  T. C. Winter,et al.  Groundwater contribution to the water and chemical budgets of Williams Lake, Minnesota, 1980–1991 , 1995 .

[20]  W. Dean,et al.  Ostracode δ18O and δ13C evidence of Holocene environmental changes in the sediments of two Minnesota lakes , 1995 .

[21]  G. Kling,et al.  Carbon Dioxide Supersaturation in the Surface Waters of Lakes , 1994, Science.

[22]  D. Hollander,et al.  A 200 year sedimentary record of progressive eutrophication in lake Greifen (Switzerland): Implications for the origin of organic-carbon-rich sediments , 1992 .

[23]  Eville Gorham,et al.  The biogeochemistry of northern peatlands and its possible responses to global warming , 1995 .

[24]  J. Lund,et al.  Some relationships between algal standing crop, water chemistry, and sediment chemistry in the English Lakes1 , 1974 .

[25]  H. Wong,et al.  Nitrogen and C/N ratios in the sediments of Lakes Superior, Huron, St. Clair, Erie, and Ontario , 1977 .