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亚马逊森林生态系统中的养分动态:I. 细凋落物中的养分通量及养分利用效率

Nutrient dynamics within amazonian forest ecosystems : I. Nutrient flux in fine litter fall and efficiency of nutrient utilization.

作者信息

Cuevas E, Medina E

机构信息

Centro de Ecologia, Instituto Venezolano de Investigaciones Cientificas, Aptdo. 1827, 1010A, Caracas, Venezuela.

出版信息

Oecologia. 1986 Sep;68(3):466-472. doi: 10.1007/BF01036756.

Abstract

A comparative analysis on the rate of fine litterfall and its associated nutrient fluxes was carried out in a mixed forest on Tierra Firme, a tall Amazon Caatinga and a Bana on podsolized sands near San Carlos de Rio Negro. There was seasonality in leaf fall and total litterfall in mixed forest and tall Amazon Caatinga forest but no definite trend in the Bana. Litterfall curves were significantly correlated among sites indicating common regulating factors in the three forests. Leaf litter from mixed forest on Tierra Firme was richer in N with extremely low Ca and Mg concentrations; tall Amazon Caatinga litter had higher P and Mg concentration, while Bana litter was low in N but K concentration was twice as high as in the other two forests. Annual fine litterfall in Tierra Firme mixed forest was nearly 4 times higher than in Bana, But N flux was 10 times higher, while Ca and Mg fluxes were similar. Tall Amazon Caatinga had Ca and Mg fluxes in litterfall 2-3 times higher than the other two forests. Within-stand efficiency of nitrogen, calcium and magnesium use, as measured by biomass/nutrient ratios, differentiates Tierra Firme from Caatinga and Bana forest: Tierra Firme has the lowest N, but the highest Ca and Mg use efficiencies. Higher P use efficiency was measured in Bana followed by Tierra Firme and Caatinga; while Tierra Firme and Caatinga showed similar higher K use efficiencies than Bana. N/P ratios indicates that Tierra Firme forest is limited by P availability, while low N availability predominates in Caatinga. Bana appears limited by both N and P. These differences probably relate to variations in degree of sclerophylly and leaf duration which determine leaf nutrient concentrations in the ecosystems studied.

摘要

在位于蒂拉弗尔梅的一片混交林、一片高大的亚马孙卡廷加林以及圣卡洛斯-德里奥内格罗附近发育于灰化砂上的巴纳林中,对细凋落物速率及其相关养分通量进行了比较分析。混交林和高大的亚马孙卡廷加林中的落叶和总凋落物存在季节性,但巴纳林中没有明确的趋势。各地点的凋落物曲线显著相关,表明这三种森林存在共同的调节因素。蒂拉弗尔梅混交林的落叶含氮量较高,钙和镁浓度极低;高大的亚马孙卡廷加林凋落物的磷和镁浓度较高,而巴纳林凋落物含氮量低,但钾浓度是其他两种森林的两倍。蒂拉弗尔梅混交林的年细凋落物量几乎是巴纳林的4倍,但氮通量高10倍,而钙和镁通量相似。高大的亚马孙卡廷加林凋落物中的钙和镁通量比其他两种森林高2至3倍。通过生物量/养分比衡量的林分内部氮、钙和镁的利用效率,使蒂拉弗尔梅林与卡廷加林和巴纳林区分开来:蒂拉弗尔梅林的氮利用效率最低,但钙和镁利用效率最高。巴纳林的磷利用效率较高,其次是蒂拉弗尔梅林和卡廷加林;而蒂拉弗尔梅林和卡廷加林的钾利用效率高于巴纳林,且二者相似。氮/磷比表明,蒂拉弗尔梅林受磷有效性限制,而卡廷加林以氮有效性低为主。巴纳林似乎同时受氮和磷的限制。这些差异可能与硬叶程度和叶持续时间的变化有关,这些因素决定了所研究生态系统中叶片的养分浓度。

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