Zobrazeno 1 - 10
of 13
pro vyhledávání: '"R. D. Bardgett"'
Autor:
J. M. Lavallee, M. Chomel, N. Alvarez Segura, F. de Castro, T. Goodall, M. Magilton, J. M. Rhymes, M. Delgado-Baquerizo, R. I. Griffiths, E. M. Baggs, T. Caruso, F. T. de Vries, M. Emmerson, D. Johnson, R. D. Bardgett
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-11 (2024)
Abstract Soil microbial communities are dominated by a relatively small number of taxa that may play outsized roles in ecosystem functioning, yet little is known about their capacities to resist and recover from climate extremes such as drought, or h
Externí odkaz:
https://doaj.org/article/cd86d58e5ba548a8914cbacf7673ad15
Autor:
K. Yu, J. van den Hoogen, Z. Wang, C. Averill, D. Routh, G. R. Smith, R. E. Drenovsky, K. M. Scow, F. Mo, M. P. Waldrop, Y. Yang, W. Tang, F. T. De Vries, R. D. Bardgett, P. Manning, F. Bastida, S. G. Baer, E. M. Bach, C. García, Q. Wang, L. Ma, B. Chen, X. He, S. Teurlincx, A. Heijboer, J. A. Bradley, T. W. Crowther
Publikováno v:
Earth System Science Data, Vol 14, Pp 4339-4350 (2022)
Fungi and bacteria are the two dominant groups of soil microbial communities worldwide. By controlling the turnover of soil organic matter, these organisms directly regulate the cycling of carbon between the soil and the atmosphere. Fundamental diffe
Externí odkaz:
https://doaj.org/article/37a93d10422342d9be0459c2ea6e1ee9
Autor:
J. M. Rhymes, I. Cordero, M. Chomel, J. M. Lavallee, A. L. Straathof, D. Ashworth, H. Langridge, M. Semchenko, F. T. de Vries, D. Johnson, R. D. Bardgett
Publikováno v:
SOIL, Vol 7, Pp 95-106 (2021)
It is widely accepted that the measurement of organic and inorganic forms of carbon (C) and nitrogen (N) in soils should be performed on fresh extracts taken from fresh soil samples. However, this is often not possible, and it is common practice to s
Externí odkaz:
https://doaj.org/article/522643156ede47ca97fa2a1b057ff259
Autor:
G. Key, M. G. Whitfield, J. Cooper, F. T. De Vries, M. Collison, T. Dedousis, R. Heathcote, B. Roth, S. Mohammed, A. Molyneux, W. H. Van der Putten, L. V. Dicks, W. J. Sutherland, R. D. Bardgett
Publikováno v:
SOIL, Vol 2, Iss 4, Pp 511-521 (2016)
The goal of this study is to clarify research needs and identify effective practices for enhancing soil health. This was done by a synopsis of soil literature that specifically tests practices designed to maintain or enhance elements of soil health.
Externí odkaz:
https://doaj.org/article/b701572451154fa8af20e2033e20fd5c
Autor:
S. D. Keesstra, J. Bouma, J. Wallinga, P. Tittonell, P. Smith, A. Cerdà, L. Montanarella, J. N. Quinton, Y. Pachepsky, W. H. van der Putten, R. D. Bardgett, S. Moolenaar, G. Mol, B. Jansen, L. O. Fresco
Publikováno v:
SOIL, Vol 2, Iss 2, Pp 111-128 (2016)
In this forum paper we discuss how soil scientists can help to reach the recently adopted UN Sustainable Development Goals (SDGs) in the most effective manner. Soil science, as a land-related discipline, has important links to several of the SDGs, wh
Externí odkaz:
https://doaj.org/article/8e821c95933143c5ae43f2fd51c21567
Autor:
A. T. Nottingham, B. L. Turner, J. Whitaker, N. J. Ostle, N. P. McNamara, R. D. Bardgett, N. Salinas, P. Meir
Publikováno v:
Biogeosciences, Vol 12, Iss 20, Pp 6071-6083 (2015)
Aboveground primary productivity is widely considered to be limited by phosphorus (P) availability in lowland tropical forests and by nitrogen (N) availability in montane tropical forests. However, the extent to which this paradigm applies to belowgr
Externí odkaz:
https://doaj.org/article/cff0c020d1054470b681339f23621362
Publikováno v:
Biogeosciences, Vol 8, Iss 5, Pp 1131-1139 (2011)
Plant-soil interactions are central to short-term carbon (C) cycling through the rapid transfer of recently assimilated C from plant roots to soil biota. In grassland ecosystems, changes in C cycling are likely to be influenced by land use and manage
Externí odkaz:
https://doaj.org/article/3a43e642524048ee90baed8ae80416e6
Autor:
S. D. Keesstra, J. Bouma, J. Wallinga, P. Tittonell, P. Smith, A. Cerdà, L. Montanarella, J. Quinton, Y. Pachepsky, W. H. van der Putten, R. D. Bardgett, S. Moolenaar, G. Mol, L. O Fresco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7a8feb939b19d9dc3ed8c7b88dabf59
https://doi.org/10.5194/soil-2015-88-supplement
https://doi.org/10.5194/soil-2015-88-supplement
Publikováno v:
Rapid communications in mass spectrometry : RCM. 14(15)
It is becoming increasingly apparent that soil amino acids are a principal source of nitrogen (N) for certain plants, and especially those of N-limited environments. This study of temperate upland grasslands used glycine-2-(13)C-(15)N and ((15)NH4)(2