Zobrazeno 1 - 10
of 52
pro vyhledávání: '"Randy Kolka"'
Publikováno v:
Water, Vol 16, Iss 8, p 1154 (2024)
Mercury (Hg) is a pollutant that bioaccumulates in the food web, leading to health issues in humans and other fauna. Although anthropogenic Hg deposition has decreased over the past 20 years, our watersheds continue to be sources of Hg to downstream
Externí odkaz:
https://doaj.org/article/627ee937e4b54f9c8b2b5557d9b79482
Autor:
Shaun Watmough, Spencer Gilbert-Parkes, Nathan Basiliko, Louis J Lamit, Erik A Lilleskov, Roxanne Andersen, Jhon Del Aguila-Pasquel, Rebekka E Artz, Brian W Benscoter, Werner Borken, Luca Bragazza, Stefani M Brandt, Suzanna L Bräuer, Michael A Carson, Xin Chen, Rodney A Chimner, Bev R Clarkson, Alexander R Cobb, Andrea S Enriquez, Jenny Farmer, Samantha P Grover, Charles F Harvey, Lorna I Harris, Christina Hazard, Alison M Hoyt, John Hribljan, Jyrki Jauhiainen, Sari Juutinen, Evan S Kane, Klaus-Holger Knorr, Randy Kolka, Mari Könönen, Anna M Laine, Tuula Larmola, Patrick A Levasseur, Carmody K McCalley, Jim McLaughlin, Tim R Moore, Nadia Mykytczuk, Anna E Normand, Virginia Rich, Bryce Robinson, Danielle L Rupp, Jasmine Rutherford, Christopher W Schadt, Dave S Smith, Graeme Spiers, Leho Tedersoo, Pham Q Thu, Carl C Trettin, Eeva-Stiina Tuittila, Merritt Turetsky, Zuzana Urbanová, Ruth K Varner, Mark P Waldrop, Meng Wang, Zheng Wang, Matt Warren, Magdalena M Wiedermann, Shanay T Williams, Joseph B Yavitt, Zhi-Guo Yu, Geoff Zahn
Publikováno v:
PLoS ONE, Vol 17, Iss 11, p e0275149 (2022)
Peatlands account for 15 to 30% of the world's soil carbon (C) stock and are important controls over global nitrogen (N) cycles. However, C and N concentrations are known to vary among peatlands contributing to the uncertainty of global C inventories
Externí odkaz:
https://doaj.org/article/d748b97b104f4f1ebe0d426557314932
Autor:
Mara Y McPartland, Rebecca A Montgomery, Paul J Hanson, Jana R Phillips, Randy Kolka, Brian Palik
Publikováno v:
Environmental Research Letters, Vol 15, Iss 12, p 124066 (2020)
Peatlands store a significant amount of terrestrial organic carbon in plant biomass and soils. The Spruce and Peatland Responses Under Changing Environments (SPRUCE) project is a warming and elevated carbon dioxide (eCO _2 ) experiment designed to te
Externí odkaz:
https://doaj.org/article/6a6b69a22d2b4ef6bf85bbd68002a636
Autor:
Mara Y. McPartland, Michael J. Falkowski, Jason R. Reinhardt, Evan S. Kane, Randy Kolka, Merritt R. Turetsky, Thomas A. Douglas, John Anderson, Jarrod D. Edwards, Brian Palik, Rebecca A. Montgomery
Publikováno v:
Remote Sensing, Vol 11, Iss 14, p 1685 (2019)
Peatlands, which account for approximately 15% of land surface across the arctic and boreal regions of the globe, are experiencing a range of ecological impacts as a result of climate change. Factors that include altered hydrology resulting from drou
Externí odkaz:
https://doaj.org/article/79894867846342ef8c28da09a386d7ac
Publikováno v:
Wetland Carbon and Environmental Management
The Second State of the Carbon Cycle Report (SOCCR2) culminated in 19 chapters that spanned all North American sectors – from Energy Systems to Agriculture and Land Use – known to be important for understanding carbon (C) cycling and accounting.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b84a0ed7cead6da505b6b715e4f69e43
https://doi.org/10.1002/9781119639305.ch24
https://doi.org/10.1002/9781119639305.ch24
Autor:
D. J. Brice, Natalie A. Griffiths, Stephen D. Sebestyen, Sarah J. Shelley, Randy Kolka, Colleen M. Iversen
Publikováno v:
Oikos. 2022
Bryophytes are largely responsible for globally significant carbon accumulation in peatland ecosystems. This accumulation is primarily caused by the slow decomposition of these mosses, which can be attributed to a combination of intrinsic (chemical)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be476525ae07372208b2e0a34b7025ca
https://doi.org/10.1111/oik.08584
https://doi.org/10.1111/oik.08584
Autor:
Xiaoying Shi, V. G. Salmon, Kirsten S. Hofmockel, Randy Kolka, Joel E. Kostka, Joanne Childs, Avni Malhotra, Scott D. Bridgham, D. J. Brice, Jake D. Graham, Natalie A. Griffiths, Terri M. Jicha, Jana R. Phillips, David J. Weston, Paul J. Hanson, Stephen D. Sebestyen, Jeffrey M. Warren, Anthony P. Walker, Xiaojuan Yang, Colleen M. Iversen, Richard J. Norby, Daniel M. Ricciuto, Christopher W. Schadt
Publikováno v:
Plant Soil
AIMS: Slow decomposition and isolation from groundwater mean that ombrotrophic peatlands store a large amount of soil carbon (C) but have low availability of nitrogen (N) and phosphorus (P). To better understand the role these limiting nutrients play
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d0260d38e7f7e138d30c5ef3e9e07ba
https://europepmc.org/articles/PMC9580354/
https://europepmc.org/articles/PMC9580354/
Publikováno v:
Mitigation and Adaptation Strategies for Global Change. 24:493-505
It is widely known that tropical peatlands, including peat swamp forests (PSFs), provide numerous ecosystem services in both spatial and temporal dimensions. These include their role as large stores for organic carbon, which when not managed well cou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a9fec21951956304db1636ae8f94416
https://doi.org/10.1007/s11027-019-9844-1
https://doi.org/10.1007/s11027-019-9844-1
Autor:
Stephen Sebestyen, Robert Slesak, Anna Stockstad, Randy Kolka, Charlie Blinn, Alan Toczydlowski
Publikováno v:
Forests; Volume 13; Issue 8; Pages: 1194
It is critical to gain insight into the responses of forest soils to the changing climate. We simulated future climate conditions with growing season throughfall reduction (by 50%) and winter snow removal using a paired-plot design across a soil drai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9f4ad63e006520479d74efce498a546a
https://doi.org/10.3390/f13081194
https://doi.org/10.3390/f13081194
Autor:
Edward A. Nater, Andrew Margenot, Randy Kolka, Karis J. McFarlane, Nathaniel Looker, Alain F. Plante
In mountainous landscapes, rates of soil morphological and biogeochemical change during secondary forest succession (SFS) can vary widely with elevation due to gradients in water, energy, and mineral weathering status. Improved understanding of how e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e70e5011ee4a7201caaa0038420866a0
https://doi.org/10.5194/egusphere-egu2020-12354
https://doi.org/10.5194/egusphere-egu2020-12354