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Akademický článek

The whole-soil carbon flux in response to warming. (cover story)

Autor: Hicks Pries, Caitlin E. (AUTHOR) cehpries@lbl.gov, Castanha, C. (AUTHOR), Porras, R. C. (AUTHOR), Torn, M. S. (AUTHOR) mstorn@lbl.gov

Publikováno v: Science. 3/31/2017, Vol. 355 Issue 6332, p1420-1423. 4p. 1 Chart, 3 Graphs.

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Akademický článek

Response to Comment on “The whole-soil carbon flux in response to warming”.

Autor: Pries, Caitlin E. Hicks^1,2 (AUTHOR) caitlin.e.h.pries@dartmouth.edu, Castanha, C.¹ (AUTHOR), Porras, R.¹ (AUTHOR), Phillips, Claire³ (AUTHOR), Torn, M. S.¹ (AUTHOR) mstorn@lbl.gov

Publikováno v: Science. 2/23/2018, Vol. 359 Issue 6378, p1-3. 3p. 2 Graphs.

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Response to Comment on 'The whole-soil carbon flux in response to warming'

Autor: Hicks Pries, Caitlin E, Castanha, C, Porras, R, Phillips, Claire, Torn, MS

Publikováno v: Science (New York, N.Y.), vol 359, iss 6378
Pries, CEH; Castanha, C; Porras, R; Phillips, C; & Torn, MS. (2018). Response to comment on "the whole-soil carbon flux in response to warming". Science, 359(6378). doi: 10.1126/science.aao0457. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/9gc6v9tj

© The Authors. Temperature records and model predictions demonstrate that deep soils warm at the same rate as surface soils, contrary to Xiao et al.'s assertions. In response to Xiao et al.'s critique of our Q10analysis, we present the results with

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The effects of heating, rhizosphere, and depth on root litter decomposition are mediated by soil moisture

Autor: Castanha, C, Zhu, B, Hicks Pries, CE, Georgiou, K, Torn, MS

Publikováno v: Biogeochemistry., vol 137, iss 1-2
Castanha, C; Zhu, B; Hicks Pries, CE; Georgiou, K; & Torn, MS. (2018). The effects of heating, rhizosphere, and depth on root litter decomposition are mediated by soil moisture. Biogeochemistry, 137(1-2), 267-279. doi: 10.1007/s10533-017-0418-6. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/73b1r5rh

© 2017, Springer International Publishing AG, part of Springer Nature. The breakdown and decomposition of plant inputs are critical for nutrient cycling, soil development, and climate-ecosystem feedbacks, but uncertainties persist in how the rates a

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Akademický článek

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Declines in low-elevation subalpine tree populations outpace growth in high-elevation populations with warming

Autor: Conlisk, E, Castanha, C, Germino, MJ, Veblen, TT, Smith, JM, Kueppers, LM

Publikováno v: Conlisk, E; Castanha, C; Germino, MJ; Veblen, TT; Smith, JM; & Kueppers, LM. (2017). Declines in low-elevation subalpine tree populations outpace growth in high-elevation populations with warming. Journal of Ecology, 105(5), 1347-1357. doi: 10.1111/1365-2745.12750. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/5gs0580k

© 2017 The Authors. Journal of Ecology © 2017 British Ecological Society Species distribution shifts in response to climate change require that recruitment increase beyond current range boundaries. For trees with long life spans, the importance of

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Warming and provenance limit tree recruitment across and beyond the elevation range of subalpine forest

Autor: Kueppers, LM, Conlisk, E, Castanha, C, Moyes, AB, Germino, MJ, de Valpine, P, Torn, MS, Mitton, JB

Publikováno v: Global change biology, vol 23, iss 6
Kueppers, LM; Conlisk, E; Castanha, C; Moyes, AB; Germino, MJ; de Valpine, P; et al.(2017). Warming and provenance limit tree recruitment across and beyond the elevation range of subalpine forest. Global Change Biology, 23(6), 2383-2395. doi: 10.1111/gcb.13561. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/3sx5407w

© 2016 John Wiley & Sons Ltd Climate niche models project that subalpine forest ranges will extend upslope with climate warming. These projections assume that the climate suitable for adult trees will be adequate for forest regeneration, ignoring cl

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The whole-soil carbon flux in response to warming

Autor: Hicks Pries, Caitlin E, Castanha, C, Porras, RC, Torn, MS

Publikováno v: Science (New York, N.Y.), vol 355, iss 6332
Hicks Pries, CE; Castanha, C; Porras, RC; & Torn, MS. (2017). The whole-soil carbon flux in response to warming. Science, 355(6332). doi: 10.1126/science.aal1319. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/1b60g2n2

Soil organic carbon harbors three times as much carbon as Earth's atmosphere, and its decomposition is a potentially large climate change feedback and major source of uncertainty in climate projections. The response of whole-soil profiles to warming

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