Zobrazeno 1 - 10
of 227
pro vyhledávání: '"S. A. Allison"'
Autor:
E. S. Duan, L. Chavez Rodriguez, N. Hemming-Schroeder, B. Wijas, H. Flores-Moreno, A. W. Cheesman, L. A. Cernusak, M. J. Liddell, P. Eggleton, A. E. Zanne, S. D. Allison
Publikováno v:
Biogeosciences, Vol 21, Pp 3321-3338 (2024)
Deadwood is an important yet understudied carbon pool in tropical ecosystems. Deadwood degradation to CO2 through decomposer (microbial, termite) activities is driven by wood moisture and temperature, which are in turn strongly influenced by local cl
Externí odkaz:
https://doaj.org/article/d0527188b9c2488b9146de8805edbcac
Autor:
J. T. Lennon, R. Z. Abramoff, S. D. Allison, R. M. Burckhardt, K. M. DeAngelis, J. P. Dunne, S. D. Frey, P. Friedlingstein, C. V. Hawkes, B. A. Hungate, S. Khurana, S. N. Kivlin, N. M. Levine, S. Manzoni, A. C. Martiny, J. B. H. Martiny, N. K. Nguyen, M. Rawat, D. Talmy, K. Todd-Brown, M. Vogt, W. R. Wieder, E. J. Zakem
Publikováno v:
mBio, Vol 15, Iss 5 (2024)
ABSTRACTClimate change jeopardizes human health, global biodiversity, and sustainability of the biosphere. To make reliable predictions about climate change, scientists use Earth system models (ESMs) that integrate physical, chemical, and biological
Externí odkaz:
https://doaj.org/article/341c1cd6ab304cda8234fa7d083b574e
Publikováno v:
Biogeosciences, Vol 17, Pp 4043-4057 (2020)
To make predictions about the carbon cycling consequences of rising global surface temperatures, Earth system scientists rely on mathematical soil biogeochemical models (SBMs). However, it is not clear which models have better predictive accuracy, an
Externí odkaz:
https://doaj.org/article/6622f9e1a1b24090842b0d751cf10422
Publikováno v:
Journal of Geophysical Research: Biogeosciences. 128
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e42e6aaebf2b314ba7b4841d63c90bf
https://doi.org/10.1029/2022jg007234
https://doi.org/10.1029/2022jg007234
Autor:
K. E. O. Todd-Brown, J. T. Randerson, F. Hopkins, V. Arora, T. Hajima, C. Jones, E. Shevliakova, J. Tjiputra, E. Volodin, T. Wu, Q. Zhang, S. D. Allison
Publikováno v:
Biogeosciences, Vol 11, Iss 8, Pp 2341-2356 (2014)
Soil is currently thought to be a sink for carbon; however, the response of this sink to increasing levels of atmospheric carbon dioxide and climate change is uncertain. In this study, we analyzed soil organic carbon (SOC) changes from 11 Earth syste
Externí odkaz:
https://doaj.org/article/5b08768262294d159860f599deedfe00
Publikováno v:
Biogeosciences, Vol 11, Iss 6, Pp 1599-1611 (2014)
Marine microbial communities mediate many biogeochemical transformations in the ocean. Consequently, processes such as primary production and carbon (C) export are linked to nutrient regeneration and are influenced by the resource demand and elementa
Externí odkaz:
https://doaj.org/article/e4f17f13a003430abf965d2f59fe339b
Autor:
N. C. Scales, A. B. Chase, S. S. Finks, A. A. Malik, C. Weihe, S. D. Allison, A. C. Martiny, J. B. H. Martiny
Publikováno v:
Applied and Environmental Microbiology. 88
Global change experiments often observe shifts in bacterial community composition based on 16S rRNA gene sequences. However, this genetic region can mask a large amount of genetic and phenotypic variation among bacterial strains sharing even identica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::20baba5dcb9f6d6f30549ae0d546316b
https://doi.org/10.1128/aem.02429-21
https://doi.org/10.1128/aem.02429-21
Publikováno v:
Biogeosciences, Vol 10, Iss 6, Pp 4341-4356 (2013)
The elemental ratios of marine phytoplankton emerge from complex interactions between the biotic and abiotic components of the ocean, and reflect the plastic response of individuals to changes in their environment. The stoichiometry of phytoplankton
Externí odkaz:
https://doaj.org/article/a74282c122ab4e69b75bc3eb9dcb9859
Autor:
K. E. O. Todd-Brown, J. T. Randerson, W. M. Post, F. M. Hoffman, C. Tarnocai, E. A. G. Schuur, S. D. Allison
Publikováno v:
Biogeosciences, Vol 10, Iss 3, Pp 1717-1736 (2013)
Stocks of soil organic carbon represent a large component of the carbon cycle that may participate in climate change feedbacks, particularly on decadal and centennial timescales. For Earth system models (ESMs), the ability to accurately represent the
Externí odkaz:
https://doaj.org/article/6456bec4bd7c4ff4a876be7cc67a196c