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Global Change Biology · 2020 · Vol. 26 · Issue 12 · Wiley
Ben Bond‐Lamberty; Danielle S. Christianson; Avni Malhotra; Stephanie C. Pennington; Debjani Sihi; Amir AghaKouchak; Hassan Anjileli; M. Altaf Arain; Juan J. Armesto; Samaneh Ashraf; Mioko Ataka; Dennis Baldocchi; Thomas Andrew Black; Nina Buchmann; Mariah S. Carbone; Shih‐Chieh Chang; Patrick Crill; Peter S. Curtis; Eric A. Davidson; Ankur R. Desai; John E. Drake; Tarek S. El‐Madany; Michael Gavazzi; Carolyn‐Monika Görres; Christopher M. Gough; Michael Goulden; Jillian Gregg; Omar Gutiérrez del Arroyo; Jin‐Sheng He; Takashi Hirano; Anya Hopple; Holly Hughes; Järvi Järveoja; Rachhpal Jassal; Jinshi Jian; Haiming Kan; Jason Kaye; Yuji Kominami; Naishen Liang; David Lipson; Catriona A. Macdonald; Kadmiel Maseyk; Kayla Mathes; Marguerite Mauritz; Melanie A. Mayes; Steve McNulty; Guofang Miao; Mirco Migliavacca; Scott Miller; Chelcy F. Miniat; Jennifer G. Nietz; Mats B. Nilsson; Asko Noormets; Hamidreza Norouzi; Christine S. O’Connell; Bruce Osborne; Cecilio Oyonarte; Zhuo Pang; Matthias Peichl; Elise Pendall; Jorge F. Perez‐Quezada; Claire L. Phillips; Richard P. Phillips; James W. Raich; Alexandre A. Renchon; Nadine K. Ruehr; Enrique P. Sánchez‐Cañete; Matthew Saunders; Kathleen E. Savage; Marion Schrumpf; Russell L. Scott; Ulli Seibt; Whendee L. Silver; Wu Sun; Daphne Szutu; Kentaro Takagi; Masahiro Takagi; Munemasa Teramoto; Mark G. Tjoelker; Susan Trumbore; Masahito Ueyama; Rodrigo Vargas; Ruth K. Varner; Joseph Verfaillie; Christoph Vogel; Jinsong Wang; Greg Winston; Tana E. Wood; Juying Wu; Thomas Wutzler; Jiye Zeng; Tianshan Zha; Quan Zhang; Junliang Zou
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and it is critical to understand how soil greenhouse gas (GHG) emissions and uptake will respond to ongoing climate change. In particular, the soil‐to‐atmosphere CO 2 flux, commonly though imprecisely termed soil respiration ( R S ), is one of the largest carbon fluxes in the Earth system. An increasing number of high‐frequency R S...
Ecology Letters · 2019 · Vol. 22 · Issue 1 · Wiley
While forest management strongly influences biodiversity, it remains unclear how the structural and compositional changes caused by management affect different community dimensions (e.g. richness, specialisation, abundance or completeness) and how this differs between taxa. We assessed the effects of nine forest features (representing stand structure, heterogeneity and tree composition) on thirteen above‐ and belowground troph...
Global Change Biology · 2010 · Vol. 16 · Issue 5 · Wiley
Overviewing the European carbon (C), greenhouse gas (GHG), and non‐GHG fluxes, gross primary productivity (GPP) is about 9.3 Pg yr −1 , and fossil fuel imports are 1.6 Pg yr −1 . GPP is about 1.25% of solar radiation, containing about 360 × 10 18 J energy – five times the energy content of annual fossil fuel use. Net primary production (NPP) is 50%, terrestrial net biome productivity, NBP, 3%, and the net GHG balance, NGB, 0.3...
Journal of Biogeography · 2004 · Vol. 31 · Issue 6 · Wiley
Aim This study investigates diversity patterns of vascular plants and plant‐feeding geometrid moths during montane rain forest regeneration in relation to the biogeographical and historical conditions of Mt Kilimanjaro. Location Investigations were undertaken on the south‐western slopes of Mt Kilimanjaro at altitudes between 2075 and 2265 m. Methods Thirteen plots were selected for this study. Four of these were situated in th...