Biotic and Abiotic Drivers of Topsoil Organic Carbon Concentration in Drylands Have Similar Effects at Regional and Global Scales
2019
Gaitan, Juan Jose | Maestre, Fernando Tomás | Bran, Donaldo Eduardo | Buono, Gustavo Gabriel | Dougill, Andrew J. | Garcia Martinez, Guillermo Carlos | Ferrante, Daniela | Guuroh, Reginald Tang | Linstadter, Anja | Massara Paletto, Virginia | Thomas, Andrew David | Oliva, Gabriel Esteban
Drylands contain 25% of the world’s soil organic carbon (SOC), which is controlled by many factors, both abiotic and biotic. Thus, understanding how these factors control SOC concentration can help to design more sustainable land-use practices in drylands aiming to foster and preserve SOC storage, something particularly important to fight ongoing global warming. We use two independent, largescale databases with contrasting geographic coverage (236 sites in global drylands and 185 sites in Patagonia, Argentina) to evaluate the relative importance of abiotic (precipitation, temperature and soil texture) and biotic (primary productivity) factors as drivers of SOC concentration in drylands at global and regional scales. We found that biotic and abiotic factors had similar effects on SOC concentration across regional and global scales: Maximum temperature and sand content had negative effects, while precipitation and plant productivity exerted positive effects. Our findings provide empirical evidence that increases in temperature and reductions in rainfall, as forecasted by climatic models in many drylands worldwide, promote declines in SOC both directly and indirectly via the reduction in plant productivity. This has important implications for the conservation of drylands under climate change; land management should seek to enhance plant productivity as a tool to offset the negative impact of climate change on SOC storage and on associated ecosystem services.
اظهر المزيد [+] اقل [-]Estación Experimental Agropecuaria Bariloche
اظهر المزيد [+] اقل [-]Fil: Gaitan, Juan Jose. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentina. Universidad Nacional de Luján. Departamento de Tecnología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
اظهر المزيد [+] اقل [-]Fil: Maestre, Fernando T. Universidad Rey Juan Carlos. Escuela Superior de Ciencias Experimentales y Tecnología. Departamento de Biología y Geología, Física y Química Inorgánica; España
اظهر المزيد [+] اقل [-]Fil: Bran, Donaldo Eduardo. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Bariloche; Argentina
اظهر المزيد [+] اقل [-]Fil: Buono, Gustavo Gabriel. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Chubut; Argentina
اظهر المزيد [+] اقل [-]Fil: Dougill, Andrew J. University of Leeds. School of Earth and Environment; Reino Unido
اظهر المزيد [+] اقل [-]Fil: Garcia Martinez, Guillermo Carlos. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Esquel; Argentina
اظهر المزيد [+] اقل [-]Fil: Ferrante, Daniela. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Santa Cruz; Argentina
اظهر المزيد [+] اقل [-]Fil: Guuroh, Reginald Tang. CSIR-Forestry Research Institute of Ghana; Ghana
اظهر المزيد [+] اقل [-]Fil: Linstadter, Anja. University of Cologne. Botanical Institute; Alemania
اظهر المزيد [+] اقل [-]Fil: Massara Paletto, Virginia. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Chubut; Argentina
اظهر المزيد [+] اقل [-]Fil: Thomas, Andrew David. Aberystwyth University. Department of Geography and Earth Sciences; Reino Unido
اظهر المزيد [+] اقل [-]Fil: Oliva, Gabriel Esteban. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Santa Cruz; Argentina
اظهر المزيد [+] اقل [-]الكلمات المفتاحية الخاصة بالمكنز الزراعي (أجروفوك)
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