排序方式: 共有3条查询结果,搜索用时 46 毫秒
1
1.
Christian Mrz Felipe S. Freitas Johan C. Faust Jasmin A. Godbold Sian F. Henley Allyson C. Tessin Geoffrey D. Abbott Ruth Airs Sandra Arndt David K. A. Barnes Laura J. Grange Neil D. Gray Ian M. Head Katharine R. Hendry Robert G. Hilton Adam J. Reed Saskia Rühl Martin Solan Terri A. Souster Mark A. Stevenson Karen Tait James Ward Stephen Widdicombe 《Ambio》2022,51(2):370
Unprecedented and dramatic transformations are occurring in the Arctic in response to climate change, but academic, public, and political discourse has disproportionately focussed on the most visible and direct aspects of change, including sea ice melt, permafrost thaw, the fate of charismatic megafauna, and the expansion of fisheries. Such narratives disregard the importance of less visible and indirect processes and, in particular, miss the substantive contribution of the shelf seafloor in regulating nutrients and sequestering carbon. Here, we summarise the biogeochemical functioning of the Arctic shelf seafloor before considering how climate change and regional adjustments to human activities may alter its biogeochemical and ecological dynamics, including ecosystem function, carbon burial, or nutrient recycling. We highlight the importance of the Arctic benthic system in mitigating climatic and anthropogenic change and, with a focus on the Barents Sea, offer some observations and our perspectives on future management and policy. 相似文献
2.
Van Hees Patrick A. W. Jones David L. Godbold Douglas L. 《Water, Air, & Soil Pollution: Focus》2003,3(4):121-144
The effect of liming (3.45 and 8.75 t ha-1 dolomite; 16 yr after application) on the biodegradation of three low molecular weight organic acids (citrate, oxalate and propionate) in forest soils was investigated. The concentration of organic acids in the soil solution followed the series propionate > citrate > oxalate with liming having no significant impact on soil solution concentrations (mean organic acid concentration = 8.7 ± 2.3 M). Organic acid mineralization by the soil microbial community was rapid in surface organic horizons (mean half-life for citrate = 2–6 h), with biodegradation rate gradually declining with soil depth. Concentration-dependent biodegradation studies (0 to 350 M) showed that the mineralization kinetics generally conformed well to a single Michaelis–Menten equation with Vmax values following the series oxalate > citrate > propionate (mean = 9.8 ± 1.0 nmol g-1 h-1) and KM values following the series oxalate = citrate > propionate (mean 168 ± 25 M). The Vmax values declined with soil depth, which was consistent with a general reduction in microbial activity down the soil profile. Liming induced a significant increase in Vmax for citrate with no change for propionate and reduction in Vmax for oxalate. The latter was probably due to adsorption and precipitation of Ca-oxalate making it unavailable for microbial uptake. The higher adsorption/precipitation capacity for oxalate in the limed soils was confirmed by adsorption isotherms. Generally, liming increased soil microbial activity by approximately 10 to 35% with calculations based on soil solution concentrations indicating that organic acid mineralization constituted approximately 3 to 15% of the total soil respiration. 相似文献
3.
Kris Verheyen Margot Vanhellemont Harald Auge Lander Baeten Christopher Baraloto Nadia Barsoum Simon Bilodeau-Gauthier Helge Bruelheide Bastien Castagneyrol Douglas Godbold Josephine Haase Andy Hector Hervé Jactel Julia Koricheva Michel Loreau Simone Mereu Christian Messier Bart Muys Philippe Nolet Alain Paquette John Parker Mike Perring Quentin Ponette Catherine Potvin Peter Reich Andy Smith Martin Weih Michael Scherer-Lorenzen 《Ambio》2016,45(1):29-41
1