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- Recent research has linked climate warming to global declines in caribou and reindeer (both Rangifer tarandus) populations. We hypothesize large-scale climate patterns are a contributing factor explaining why these declines are not universal. To test our hypothesis for such relationships among Alaska caribou herds, we calculated the population growth rate and percent change of four arctic herds using existing population estimates, and explored associations with indices of the Arctic Oscillation (AO) and the Pacific Decadal Oscillation (PDO). The AO, which more strongly affects eastern...AuthorsKyle Joly, David Klein, David L. Verbyla, T. Scott Rupp, F. Stuart ChapinKeywordsSourceEcography. 34: 345-352Year2011
- The direction and magnitude of soil organic carbon (SOC) changes in response to climate change remain unclear and depend on the spatial distribution of SOC across landscapes. Uncertainties regarding the fate of SOC are greater in high-latitude systems where data are sparse and the soils are affected by sub-zero temperatures. To address these issues in Alaska, a first-order assessment of data gaps and spatial distributions of SOC was conducted from a recently compiled soil carbon database. Temperature and landform type were the dominant controls on SOC distribution for selected ecoregions....AuthorsKristofer Johnson, Jennifer Harden, A. David McGuire, Norman B. Bliss, James G. Bockheim, Mark Clark, Teresa Nettleton-Hollingsworth, M. Torre Jorgenson, Evan Kane, Michelle Mack, Johathan ODonnell, Chien-Lu Ping, Edward A.G. Schuur, Merritt R. Turetsky, David W. ValentineKeywordsSourceGeoderma. 167-168: 71-84Year2011
- Studies indicate that, historically, terrestrial ecosystems of the northern high-latitude region may have been responsible for up to 60% of the global net land-based sink for atmospheric C02. However, these regions have recently experienced remarkable modification of the major driving forces of the carbon cycle, including surface air temperature warming that is significantly greater than the global average and associated increases in the frequency and severity of disturbances. Whether Arctic tundra and boreal forest ecosystems will continue to sequester atmospheric C02 in the face of these...AuthorsD.J. Hayes, A.D. McGuire, D.W. Kicklighter, K.R. Gurney, T.J. Burnside, J.M. MelilloKeywordsSourceGlobal Biogeochemical Cycles. 25: GB3018. 14 p. doi: 10.1029/2010GB003813Year2011
- To develop silvicultural strategies for restoring longleaf pine (Pinus palustris Mill.) savannas, mortality and growth of overstory pines and midstory hardwoods and abundance and species richness of herbs were studied for 14 years after pine thinning and nonpine woody control. Pine cover in thinned stands was about half of that in nonthinned stands through year 5, but it lagged by only 8% and 3% in years 9 and 14, respectively, because of vigorous crown responses. Despite a cumulative mortality of 64% of hardwood stems from prescribed fires in years 0, 4, and 9, hardwood basal area in...AuthorsTimothy B. HarringtonKeywordsSourceCanadian Journal of Forestry Research. 41: 2301-2314Year2011
- Permafrost deposits constitute a large organic carbon pool highly vulnerable to degradation and potential carbon release due to global warming. Permafrost sections along coastal and river bank exposures in NE Siberia were studied for organic matter (OM) characteristics and ice content. OM stored in Quaternary permafrost grew, accumulated, froze, partly decomposed, and refroze under different periglacial environments, reflected in specific biogeochemical and cryolithological features. OM in permafrost is represented by twigs, leaves, peat, grass roots, and plant detritus. The vertical...AuthorsLutz Schirrmeister, Guido Grosse, Sebastian Wetterich, Pier Paul Overduin, Jens Straub, Edward A.G. Schuur, Hans-Wolfgang HubbertonKeywordsSourceJournal of Geophysical Research. 116: G00M02. 16 p. doi:10.1029/2011JG001647.Year2011
- Arctic temperatures are rising fast, and permafrost is thawing. Carbon released into the atmosphere from permafrost soils will accelerate climate change, but the magnitude of this effect remains highly uncertain. Our collective estimate is that carbon will be released more quickly than models suggest, and at levels that are cause for serious concern. We calculate that permafrost thaw will release the same order of magnitude of carbon as deforestation if current rates of deforestation continue. But because these emissions include significant quantities of methane, the overall effect on...AuthorsE.A.G. Schuur, B.W. Abbott, W.B. Bowden, V. Brovkin, P. Camill, J.P. Canadell, F.S. Chapin, T.R. Christensen, J.P. Chanton, P. Ciais, P.M. Crill, B.T. Crosby, C.I. Czimczik, G. Grosse, D.J. Hayes, G. Hugelius, J.D. Jastrow, T. Kleinen, C.D. Koven, G. Krinner, P. Kuhry, D.M. Lawrence, S.M. Natali, C.L. Ping, A. Rinke, W.J. Riley, V.E. Romanovsky, A.B.K. Sannel, C. Schadel, K. Schaefer, Z.M. Subin, C. Tarnocai, M. Turetsky, K. M. Walter-Anthony, C.J. Wilson, S.A. ZimovSourceHigh risk of permafrost thaw. Nature. 480: 32-33Year2011
- We present methodology for assessing browse removal to help evaluate resource limitation among moose Alces alces populations in large, potentially remote areas of boreal forest. During 2000-2007, we compared proportional removal (ratio of browse consumption to browse production) in eight areas of lnterior Alaska, USA, with multi-year twinning rates of the respective moose populations. Several prior studies concluded that twinning rate provided an index of the nutritional condition of moose. We theorized that a plant-based sampling of proportional use of browse by moose in late winter would...AuthorsC.Tom Seaton, Thomas F. Paragi, Rodney D. Boertje, Knut Kielland, Stephen DuBois, Craig L. FleenerKeywordsSourceWildlife Biology. 17(1): 55-66Year2011
- We assessed changes in mineral soil total carbon (C) and nutrient (exchangeable Ca, K, Mg, and total N) pools to 60 cm depth 5 years after manipulating biomass and competing vegetation at two contrasting Douglas-fir plantations (Matlock, WA, and Molalla, OR). Biomass treatments included whole-tree (WT) and bole-only (BO) harvest, and competing vegetation control (VC) treatments were applied as either initial or annual herbicide applications. There were main effects of biomass removal and VC on the absolute change in soil pools of some elements at both sites, but significant effects were...AuthorsRobert A. Slesak, Stephen H. Schoenholtz, Timothy B. HarringtonKeywordsSourceForest Ecology and Management. 262: 1722-1728Year2011
- Current evidence from temperate studies suggests that ectomycorrhizal (ECM) fungi require overland routes for migration because of their obligate symbiotic associations with woody plants. Despite their key roles in arctic ecosystems, the phylogenetic diversity and phylogeography of arctic ECM fungi remains little known. Here we assess the phylogenetic diversity of ECM communities in an isolated, formerly glaciated, high arctic archipelago, and provide explanations for their phylogeographic origins. Our results indicate numerous recent colonization events and suggest that long-distance,...AuthorsJ. Geml, I. Timling, C.H. Robinson, N. Lennon, H.C. Nusbaum, C. Brochmann, M.E. Noordeloos, D.L. TaylorKeywordsSourceJournal of Biogeography. 39: 74-88. doi: 1 0.1111/j.1365-2699.20 11 02588.xYear2011
- Information on land cover at global and continental scales is critical for addressing a range of ecological, socioeconomic and policy questions. Global land cover maps have evolved rapidly in the last decade, but efforts to evaluate map uncertainties have been limited, especially in remote areas like Northern Eurasia. Northern Eurasia comprises a particularly diverse region covering a wide range of climate zones and ecosystems: from arctic deserts, tundra, boreal forest, and wetlands, to semi-arid steppes and the deserts of Central Asia. In this study, we assessed four of the most recent...AuthorsDirk Pflugmacher, Olga N. Krankina, Warren B. Cohen, Mark A. Friedl, Damien Sulla-Menashe, Robert Kennedy, Peder Nelson, Tatiana V. Loboda, Tobias Kuemmerle, Egor Dyukarev, Vladimir Elsadov, Viacheslav I. KharukKeywordsSourceRemote Sensing of Environment. 115: 3539-3553Year2011