FN Archimer Export Format PT J TI Atmospheric deposition of elements and its relevance for nutrient budgets of tropical forests BT AF Van Langenhove, Leandro Verryckt, Lore T. Bréchet, Laëtitia Courtois, Elodie A. Stahl, Clement Hofhansl, Florian Bauters, Marijn Sardans, Jordi Boeckx, Pascal Fransen, Erik Peñuelas, Josep Janssens, Ivan A. AS 1:1;2:1;3:1;4:2;5:3;6:4;7:5;8:6,7;9:5;10:8,9;11:6,7;12:1; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:; C1 Centre of Excellence PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Wilrijk, Belgium Laboratoire Ecologie, évolution, Interactions des Systèmes Amazoniens (LEEISA), Université de Guyane, CNRS, IFREMER, French Guiana, 97300, Cayenne, France INRA, UMR EcoFoG, CNRS, Cirad, AgroParisTech, Université des Antilles, Université de Guyane, 97387, Kourou, France International Institute for Applied Systems Analysis (IIASA), Schlossplatz 1, 2361, Laxenburg, Austria Isotope Bioscience Laboratory–ISOFYS, Ghent University, 9000, Gent, Belgium CSIC, Global Ecology Unit CREAF-CSIC-UAB, 08193, Bellaterra, Catalonia, Spain CREAF, 08193, Cerdanyola del Vallès, Catalonia, Spain Center of Medical Genetics, University of Antwerp, Prins Boudewijnlaan 43/6, 2650, Edegem, Antwerp, Belgium StatUa Center for Statistics, University of Antwerp, Prinsstraat 13, 2000, Antwerp, Belgium C2 UNIV ANTWERP, BELGIUM UNIV GUYANE, FRANCE INRA, FRANCE IIASA, AUSTRIA UNIV GHENT, BELGIUM CSIC, SPAIN CREAF, SPAIN UNIV ANTWERP, BELGIUM UNIV ANTWERP, BELGIUM UM LEEISA IN WOS Cotutelle UMR copubli-france copubli-europe IF 4.825 TC 31 UR https://archimer.ifremer.fr/doc/00629/74123/73572.pdf LA English DT Article DE ;Throughfall;Litterfall;Nutrient cycling;Nitrogen;Phosphorus;Potassium AB Atmospheric deposition is an important component of the nutrient cycles of terrestrial ecosystems, but field measurements are especially scarce in tropical regions. In this study we analysed 15 months of precipitation chemistry collected in an old growth tropical forest located in French Guiana. We measured nutrient inputs via bulk precipitation and throughfall and used the canopy budget model to estimate nutrient fluxes via canopy exchange and dry deposition. Based on this method we quantified net fluxes of macronutrients and compared their contribution to internal cycling rates via litterfall. Our results suggest that while atmospheric deposition of nitrogen was relatively high (13 kg ha−1 year−1), and mainly in organic forms, the N inputs via litterfall were an order of magnitude higher. In contrast to nitrogen, we found that atmospheric deposition of phosphorus (0.5 kg ha−1 year−1) supplied up to one third of the annual litterfall input to the forest floor. Most strikingly, combined annual inputs of potassium via atmospheric deposition (14 kg ha−1 year−1) and canopy leaching (22 kg ha−1 year−1) were three times larger than internal nutrient recycling via litterfall (11 kg ha−1 year−1). We conclude that atmospheric deposition of phosphorus and especially potassium may play an important role in sustaining the productivity of this old-growth tropical rainforest. PY 2020 PD JUL SO Biogeochemistry SN 0168-2563 PU Springer Science and Business Media LLC VL 149 IS 2 UT 000532097400001 BP 175 EP 193 DI 10.1007/s10533-020-00673-8 ID 74123 ER EF