| Literature DB >> 31341281 |
Johan van den Hoogen1, Stefan Geisen2,3, Devin Routh2, Howard Ferris4, Walter Traunspurger5, David A Wardle6, Ron G M de Goede7, Byron J Adams8, Wasim Ahmad9, Walter S Andriuzzi10, Richard D Bardgett11, Michael Bonkowski12, Raquel Campos-Herrera13, Juvenil E Cares14, Tancredi Caruso15, Larissa de Brito Caixeta14, Xiaoyun Chen16, Sofia R Costa17, Rachel Creamer7, José Mauro da Cunha Castro18, Marie Dam19, Djibril Djigal20, Miguel Escuer21, Bryan S Griffiths22, Carmen Gutiérrez21, Karin Hohberg23, Daria Kalinkina24, Paul Kardol25, Alan Kergunteuil26, Gerard Korthals3, Valentyna Krashevska27, Alexey A Kudrin28, Qi Li29, Wenju Liang29, Matthew Magilton15, Mariette Marais30, José Antonio Rodríguez Martín31, Elizaveta Matveeva24, El Hassan Mayad32, Christian Mulder33, Peter Mullin34, Roy Neilson35, T A Duong Nguyen12,36, Uffe N Nielsen37, Hiroaki Okada38, Juan Emilio Palomares Rius39, Kaiwen Pan40, Vlada Peneva41, Loïc Pellissier42,43, Julio Carlos Pereira da Silva44, Camille Pitteloud42, Thomas O Powers34, Kirsten Powers34, Casper W Quist45,46, Sergio Rasmann47, Sara Sánchez Moreno48, Stefan Scheu27,49, Heikki Setälä50, Anna Sushchuk24, Alexei V Tiunov51, Jean Trap52, Wim van der Putten3,46, Mette Vestergård53, Cecile Villenave52,54, Lieven Waeyenberge55, Diana H Wall10, Rutger Wilschut3, Daniel G Wright56, Jiue-In Yang57, Thomas Ward Crowther58.
Abstract
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.Entities:
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Year: 2019 PMID: 31341281 DOI: 10.1038/s41586-019-1418-6
Source DB: PubMed Journal: Nature ISSN: 0028-0836 Impact factor: 49.962