TY - JOUR A1 - Oeser, Ralf Andreas A1 - Stroncik, Nicole A1 - Moskwa, Lisa-Marie A1 - Bernhard, Nadine A1 - Schaller, Mirjam A1 - Canessa, Rafaella A1 - van den Brink, Liesbeth A1 - Köster, Moritz A1 - Brucker, Emanuel A1 - Stock, Svenja A1 - Pablo Fuentes, Juan A1 - Godoy, Roberto A1 - Javier Matus, Francisco A1 - Oses Pedraza, Romulo A1 - Osses McIntyre, Pablo A1 - Paulino, Leandro A1 - Seguel, Oscar A1 - Bader, Maaike Y. A1 - Boy, Jens A1 - Dippold, Michaela A. A1 - Ehlers, Todd A1 - Kühn, Peter A1 - Kuzyakov, Yakov A1 - Leinweber, Peter A1 - Scholten, Thomas A1 - Spielvogel, Sandra A1 - Spohn, Marie A1 - Ubernickel, Kirstin A1 - Tielbörger, Katja A1 - Wagner, Dirk A1 - von Blanckenburg, Friedhelm T1 - Chemistry and microbiology of the Critical Zone along a steep climate and vegetation gradient in the Chilean Coastal Cordillera JF - Catena : an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution N2 - From north to south, denudation rates from cosmogenic nuclides are similar to 10 t km(-2) yr(-1) at the arid Pan de Aziicar site, similar to 20 t km(2) yr(-1) at the semi-arid site of Santa Gracia, -60 t km(-2) yr(-1) at the Mediterranean climate site of La Campana, and similar to 30 t km(-2) yr(-1) at the humid site of Nahuelbuta. A and B horizons increase in thickness and elemental depletion or enrichment increases from north (similar to 26 degrees S) to south (similar to 38 degrees S) in these horizons. Differences in the degree of chemical weathering, quantified by the chemical depletion fraction (CDF), are significant only between the arid and sparsely vegetated site and the other three sites. Differences in the CDF between the sites, and elemental depletion within the sites are sometimes smaller than the variations induced by the bedrock heterogeneity. Microbial abundances (bacteria and archaea) in saprolite substantially increase from the arid to the semi-arid sites. With this study, we provide a comprehensive dataset characterizing the Critical Zone geochemistry in the Chilean Coastal Cordillera. This dataset confirms climatic controls on weathering and denudation rates and provides prerequisites to quantify the role of biota in future studies. KW - Weathering KW - Denudation KW - Microbial abundance KW - Climate KW - Chile Y1 - 2018 U6 - https://doi.org/10.1016/j.catena.2018.06.002 SN - 0341-8162 SN - 1872-6887 VL - 170 SP - 183 EP - 203 PB - Elsevier CY - Amsterdam ER -