Title Interannual $CO_{2}$ exchange of a sparse Mediterranean shrubland on a carbonaceous substrate Author Serrano-Ortiz, P. Domingo, F. Cazorla, A. Were, A. Cuezva, S. Villagarcia, L. Alados-Arboledas, L. Kowalski, A.S. Faculty/Department Faculty of Sciences. Biology Publication type article Publication 2009 2009 Subject Physics Chemistry Biology Source (journal) Journal of geophysical research : biogeosciences Volume/pages 114(2009) , p. G04015,1-G04015,11 ISSN 0148-0227 Article Reference G04015 ISI 000272444500001 Carrier E-only publicatie Target language English (eng) Full text (Publishers DOI) Affiliation University of Antwerp Abstract This study presents the interannual CO(2) exchange of a semiarid shrubland overlying a carbonaceous substrate where abiotic processes may interact with biological processes in the ecosystem carbon cycle. Estimated by the eddy covariance technique and two different gap-filling models (RBF neural network and MDS Marginal Distribution Sampling''), the mean annual net ecosystem exchange (NEE) of CO(2) varied from -63 to 29 g C m(-2), averaging -2 +/- 23 g C m(-2) from May 2004 to December 2007. In addition, CO(2) exchange was divided into periods likely dominated by clear signals of biological activity (high daytime uptake, low Bowen ratio) and periods of apparent plant senescence (dry conditions) to better understand the relative contributions of biological versus abiotic processes'' to the annual NEE and the interannual variability of these processes. During biological periods, CO(2) exchange appears to be related to changes in the ecosystem leaf area index, whereas abiotic fluxes are most closely related to evapotranspiration. The timing of rainfall events seems to be a main determinant of both activation and duration of biological processes. During apparent abiotic periods, CO(2) exchange is characterized by daytime emissions averaging 1.5 mu mol m(-2) s(-1), whereas biological periods are characterized by daytime CO(2) uptake with mean values of around 1.4 mu mol m(-2) s(-1). As a preliminary result, the abiotic period characterized from 19% of 2004 to 45% of 2007 with a mean duration of approximately 2 months. However, future research is needed in order to achieve a more reliable division between determinant processes involved in CO(2) exchange over carbonaceous substrates. E-info http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000272444500001&DestLinkType=RelatedRecords&DestApp=ALL_WOS&UsrCustomerID=ef845e08c439e550330acc77c7d2d848 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000272444500001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=ef845e08c439e550330acc77c7d2d848 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000272444500001&DestLinkType=CitingArticles&DestApp=ALL_WOS&UsrCustomerID=ef845e08c439e550330acc77c7d2d848 Handle