Sebastian Seibold, Werner Rammer, Torsten Hothorn, Rupert Seidl, Michael D Ulyshen, Janina Lorz, Marc W Cadotte, David B Lindenmayer, Yagya P Adhikari, Roxana Aragón, Soyeon Bae, Petr Baldrian, Hassan Barimani Varandi, Jos Barlow, Claus Bässler, Jacques Beauchêne, Erika Berenguer, Rodrigo S Bergamin, Tone Birkemoe, Gergely Boros, Roland Brandl, Hervé Brustel, Philip J Burton, Yvonne T Cakpo-Tossou, Jorge Castro, Eugénie Cateau, Tyler P Cobb, Nina Farwig, Romina D Fernández, Jennifer Firn, Kee Seng Gan, Grizelle González, Martin M Gossner, Jan C Habel, Christian Hébert, Christoph Heibl, Osmo Heikkala, Andreas Hemp, Claudia Hemp, Joakim Hjältén, Stefan Hotes, Jari Kouki, Thibault Lachat, Jie Liu, Yu Liu, Ya-Huang Luo, Damasa M Macandog, Pablo E Martina, Sharif A Mukul, Baatarbileg Nachin, Kurtis Nisbet, John O'Halloran, Anne Oxbrough, Jeev Nath Pandey, Tomáš Pavlíček, Stephen M Pawson, Jacques S Rakotondranary, Jean-Baptiste Ramanamanjato, Liana Rossi, Jürgen Schmidl, Mark Schulze, Stephen Seaton, Marisa J Stone, Nigel E Stork, Byambagerel Suran, Anne Sverdrup-Thygeson, Simon Thorn, Ganesh Thyagarajan, Timothy J Wardlaw, Wolfgang W Weisser, Sungsoo Yoon, Naili Zhang, Jörg Müller
The amount of carbon stored in deadwood is equivalent to about 8 per cent of the global forest carbon stocks1 . The decomposition of deadwood is largely governed by climate2-5 with decomposer groups-such as microorganisms and insects-contributing to variations in the decomposition rates2,6,7 . At the global scale, the contribution of insects to the decomposition of deadwood and carbon release remains poorly understood7 . Here we present a field experiment of wood decomposition across 55 forest sites and 6 continents...
September 2021: Nature