不同生态系统中大型植物-附生植物复合体DOC释放的定量贡献

M. Demarty, A. Parkes, Y. Prairie
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引用次数: 0

摘要

陆地溶解有机碳(DOC)的负荷对湖泊生态系统的能量通路有重要贡献(TRANVIK 1992, PACE et al. 2004, CARPENTER et al. 2005, KRITZBERG et al. 2006)。然而,水柱代谢也可以通过底栖生物的生产来维持,因为底栖生物的生产通常主导着系统的整体生产力,特别是在浅湖中(VADEBONCOEUR等人,2003)。已知活的大型植物释放DOC (WETZEL & MANNY 1972, GoDMAIRE & NALEWAJKO 1989, BARRÓN et al. 2003),是水柱代谢的潜在碳源;因此,我们确定了活的大型植物释放的DOC总量对整个DOC库的相对贡献,以估计其在生态系统尺度上对代谢的潜在贡献。我们测量了大型植物-附生植物复合体(Demarty和Prairie, unpubl)的原位DOC释放率,并将其与流域的DOC负荷进行了比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Quantitative contribution of DOC release by the macrophyte-epiphyte complex in different ecosystems
The loading of terrestrial dissolved organic carbon (DOC) can contribute significantly to the energy pathways of lake ecosystems (TRANVIK 1992, PACE et al. 2004, CARPENTER et al. 2005, KRITZBERG et al. 2006). Water column metabolism could also be sustained by benthic production, however, because i t often dominates the overall productivity o f the system, particularly in shallow lakes (VADEBONCOEUR et al. 2003). Living macrophytes are known to release DOC (WETZEL & MANNY 1972, GoDMAIRE & NALEWAJKO 1989, BARRÓN et al. 2003) and area potential source of carbon for water column metabolism; therefore, we determined the relative contribution oftotal quantity ofDOC released by living macrophytes to the entire DOC pool to estimate its potential contribution to metabolism at the ecosystem scale. We measured in situ DOC release rates by the macrophyte-epiphyte complex (Demarty and Prairie, unpubl) and compared them to DOC loads from the watersheds.
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