Subfossil cladocerans as quantitative indicators of past ecological conditions in Yangtze River Basin lakes, China
Subfossil cladocerans as quantitative indicators of past ecological conditions in Yangtze River Basin lakes, China
复制标题
枝角亚化石作为中国长江流域湖泊过去生态状况的定量指标
DOI:
10.1016/j.scitotenv.2020.138794
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发表时间:
2020-08-01
影响因子:
9.8
通讯作者:
Jeppesen, Erik
中科院分区:
文献类型:
--
作者:
Dong, Xuhui;Kattel, Giri;Jeppesen, Erik
Cladocerans (Crustacea: Branchiopoda) are an essential component of the food webs of shallow lakes. However, their potential significance as sentinels of environmental change in subtropical regions of South-East Asia, is not well elucidated. In this study, we examined the distribution pattern of cladoceran subfossils in the surface sediments of 64 shallow lakes located in the middle and lower reaches of the Yangtze River Basin (MLYB). Using constrained ordination and multivariate regression trees (MRT), we explored the relationships between the distribution of cladocerans and contemporary environmental variables. The results indicated that macrophyte abundance is the most important regulator, followed by chlorophyllaand total phosphorus that all were important drivers of cladoceran community dynamics. Despite intensive aquaculture in the MLYB lakes over the past decades, fish predation did not have a significant influence on the cladoceran community, likely because the fish predation pressure was generally high. The MRT analysis showed distinct variations in the composition of cladoceran communities and was able to identify the key indicator species of various stressors, includingBosmina coregoni,smallAlona(A. intermedia, A. rectangula) andLeydigia acanthocercoides, Leydigia leydigiandChydorus sphaericus. Boosted Regression Tree (BRT), a novel numerical model, was employed to establish the quantitative relationship between cladoceran composition and environmental variables. The model was used to reconstruct historical macrophyte coverage over the past 60 years in a typical Yangtze lake, Liangzi Lake, based on sedimentary cladoceran records. The BRT-inferred macrophyte coverage was validated well by the macrofossil records in the same lake. Using subfossil cladocerans as indicator of the past environmental change in MLYB lakes is potentially useful given their key ecological roles. However, caution should be taken due to species-specific differences in preservation in the sediment and confounding environmental processes that to some extent may bias the conclusions.