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  • 1
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    PANGAEA
    In:  Supplement to: Gorham, Eville; Lehman, Clarence; Dyke, Arthur; Clymo; Janssens, Jan (2012): Long-term carbon sequestration in North American peatlands. Quaternary Science Reviews, 58, 77-82, https://doi.org/10.1016/j.quascirev.2012.09.018
    Publication Date: 2023-02-08
    Description: Peatland ecosystems store about 500-600 Pg of organic carbon, largely accumulated since the last glaciation. Whether they continue to sequester carbon or release it as greenhouse gases, perhaps in large amounts, is important in Earth's temperature dynamics. Given both ages and depths of numerous dated sample peatlands, their rate of carbon sequestration can be estimated throughout the Holocene. Here we use average values for carbon content per unit volume, the geographical extent of peatlands, and ecological models of peatland establishment and growth, to reconstruct the time-trajectory of peatland carbon sequestration in North America and project it into the future. Peatlands there contain ~163 Pg of carbon. Ignoring effects of climate change and other major anthropogenic disturbances, the rate of carbon accumulation is projected to decline slowly over millennia as reduced net carbon accumulation in existing peatlands is largely balanced by new peatland establishment. Peatlands are one of few long-term terrestrial carbon sinks, probably important for global carbon regulation in future generations. This study contributes to a better understanding of these ecosystems that will assist their inclusion in earth-system models, and therefore their management to maintain carbon storage during climate change.
    Keywords: Calendar age; DEPTH, sediment/rock; Identification; LATITUDE; LONGITUDE; MULT; Multiple investigations; North_American_Peatlands; Number
    Type: Dataset
    Format: text/tab-separated-values, 6183 data points
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  • 2
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    PANGAEA
    In:  Supplement to: Gorham, Eville; Swaine, Dalway J (1965): The influence of oxidizing and reducing conditions upon the distribution of some elements in lake sediments. Limnology and Oceanography, 10(2), 268-279, https://doi.org/10.4319/lo.1965.10.2.0268
    Publication Date: 2024-02-26
    Description: Analyses for Fe, Mn, Pb, Zn, Co, P, Mo, Ba, Sr, Ti, Li, Rb, Na, K, Be, Cr, V, Y, Ag, Cu, C, S, Sn, Ni, Ga, Zr, and La have been carried out on some oxidate crusts, oxidized surface muds, reduced subsurface muds, and glacial clays collected in Windermere and Esthwaite Water in the English Lake District. The relatively organic lake muds exhibit the highest concentrations of C, S, Cu, Sn, and Ni. Many of the oxidate crusts exhibit strong enrichment in Mn, Fe, Ba, Sr, Pb, and Zn. Ti, Li, Rb, Co, P, and Mo are also enriched in some crusts. S, Sn, and Ni reach their highest levels in the reducing subsurface muds, but Mn, and to a lesser extent Fe and Mo, are higher in the oxidized than in the reduced muds. Relations between the elements in the various sediments are examined, and the English oxidate crusts are compared with lake and stream ores in Sweden and Finland, and with marine manganese nodules. These marine nodules are frequently enriched in Cu, Ni, Co, Mo, V, Ag, and Sn to a far higher degree than the freshwater ferromanganese concretions. Some freshwater crusts exhibit enrichments in Pb, Zn, and Ba of the same order as those observed in marine manganese nodules.
    Keywords: Barium; Boron; Carbon, organic, total; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Flame photometry; Gallium; Identification; Iron; Lake Ullswater, United Kingdom; Lake Windermere, United Kingdom; Lanthanum; Lead; Lithium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Rubidium; Silver; Sodium; Spectrophotometer (Unicam SP500); Spectroscopy, cathode layer arc; Strontium; Sulfur, total; Tin; Titanium; Ullswater_G; Vanadium; Wet chemistry; Windermere_G; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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