作者
Johan van den Hoogen,Stefan Geisen,Devin Routh,Howard Ferris,Walter Traunspurger,David A. Wardle,R.G.M. de Goede,Byron J. Adams,Wasim Ahmad,Walter S. Andriuzzi,Richard D. Bardgett,Michael Bonkowski,Raquel Campos–Herrera,Juvenil Enrique Cares,Tancredi Caruso,Larissa de Brito Caixeta,Xiaoyun Chen,Sofia R. Costa,Rachel Creamer,J. M. da C. e Castro,Marie Dam,Djibril Djigal,Miguel Escuer,Bryan S. Griffiths,Carmen Gutiérrez,Karin Hohberg,D. S. Kalinkina,Paul Kardol,Alan Kergunteuil,G.W. Korthals,Valentyna Krashevska,Alexey A. Kudrin,Qi Li,Wenju Liang,Matthew Magilton,Mariette Marais,José Antonio Rodríguez Martín,Е. М. Матвеева,El Hassan Mayad,Christian Mulder,Peter Mullin,Roy Neilson,Thi Anh Duong Nguyen,Uffe N. Nielsen,Hiroaki Okada,Juan E. Palomares‐Rius,Kaiwen Pan,Vlada Peneva,Loïc Pellissier,Júlio Carlos Pereira da Silva,Camille Pitteloud,Thomas O. Powers,Kirsten Powers,Casper W. Quist,Sergio Rasmann,Sara Sánchez‐Moreno,Stefan Scheu,Heikki Setälä,А. А. Сущук,Alexei V. Tiunov,Jean Trap,Wim H. van der Putten,Mette Vestergård,Cécile Villenave,Lieven Waeyenberge,Diana H. Wall,Rutger A. Wilschut,Daniel G. Wright,Jiue-in Yang,Thomas W. Crowther
摘要
Soil organisms are a crucial part of the terrestrial biosphere. Despite their importance for ecosystem functioning, few quantitative, spatially explicit models of the active belowground community currently exist. In particular, nematodes are the most abundant animals on Earth, filling all trophic levels in the soil food web. Here we use 6,759 georeferenced samples to generate a mechanistic understanding of the patterns of the global abundance of nematodes in the soil and the composition of their functional groups. The resulting maps show that 4.4 ± 0.64 × 1020 nematodes (with a total biomass of approximately 0.3 gigatonnes) inhabit surface soils across the world, with higher abundances in sub-Arctic regions (38% of total) than in temperate (24%) or tropical (21%) regions. Regional variations in these global trends also provide insights into local patterns of soil fertility and functioning. These high-resolution models provide the first steps towards representing soil ecological processes in global biogeochemical models and will enable the prediction of elemental cycling under current and future climate scenarios.