Warm and fertile sub-humid conditions enhance litterfall to sustain high soil respiration fluxes in a Mediterranean cork oak forest

被引:0
作者
Zribi, Lobna [1 ,2 ]
Mouillot, Florent [3 ]
Gharbi, Fatma [1 ,2 ]
Ourcival, Jean-Marc [3 ]
Hanchi, Belgacem [2 ]
机构
[1] Institut National de Recherche en Génie Rural, Eaux et Forets. BP 10, Rue Hedi El Karray El Menzah IV, Ariana,2080, Tunisia
[2] Faculté des Sciences de Tunis, Département de Biologie, Campus Universitaire El Manar, Tunis,2092, Tunisia
[3] CEFE, UMR 5175, CNRS-Université de Montpellier-Université Paul-Valéry Montpellier-EPHE-IRD 1919, route de Mende, Montpellier 5,34293, France
关键词
Ecosystems - Soil moisture - Forestry - Budget control;
D O I
10.3390/ma8085257
中图分类号
学科分类号
摘要
Soil respiration is a major component of the global carbon budget and Mediterranean ecosystems have usually been studied in locations with shallow soils, mild temperatures, and a prolonged dry season. This study investigates seasonal soil respiration rates and underlying mechanisms under wetter, warmer, and more fertile conditions in a Mediterranean cork oak forest of Northern Tunisia (Africa), acknowledged as one of the most productive forests in the Mediterranean basin. We applied a soil respiration model based on soil temperature and relative water content and investigated how ecosystem functioning under these favorable conditions affected soil carbon storage through carbon inputs to the soil litter. Annual soil respiration rates varied between 1774 gC m-2 year-1 and 2227 gC m-2 year-1, which is on the highest range of observations under Mediterranean climate conditions. We attributed this high soil carbon flux as a response to favorable temperatures and soil water content, but this could be sustained only by a small carbon allocation to roots (root/shoot ratio = 0.31-0.41) leading to a large allocation to leaves with a multiannual leaf production, enhanced annual twig elongation (11.5-28.5 cm) with a reduced leaf life span (-2 year-1). Thus, the favorable climatic and edaphic conditions experienced by these Mediterranean cork oak forests drove high soil respiration fluxes which balanced the high carbon assimilation leading to a relatively small overall contribution (10.96-14.79 kgC m-2) to soil carbon storage. © 2015 by the authors.
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页码:5508 / 5525
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