Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils

In palaeolimnology, microfossils play an important role as ecological indicators of lake history. A reliable interpretation of microfossil data requires a comprehensive understanding of transport processes as well as determining whether microfossil assemblages are representative of their living comm...

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Main Authors: Xin Mao, Xingqi Liu, Junfeng Li, Shengnan Feng, Gaolei Jiang, Linjing Liu
Format: Article
Language:English
Published: Elsevier 2021-11-01
Series:Ecological Indicators
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1470160X21008475
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author Xin Mao
Xingqi Liu
Junfeng Li
Shengnan Feng
Gaolei Jiang
Linjing Liu
author_facet Xin Mao
Xingqi Liu
Junfeng Li
Shengnan Feng
Gaolei Jiang
Linjing Liu
author_sort Xin Mao
collection DOAJ
description In palaeolimnology, microfossils play an important role as ecological indicators of lake history. A reliable interpretation of microfossil data requires a comprehensive understanding of transport processes as well as determining whether microfossil assemblages are representative of their living communities. The occurrence of transport in ostracod taphocoenoses can be identified from the population age structure of valves. In this study, 23 surface sediment samples from Dalongchi Lake, northwestern China, were analysed for species composition, and 16 were also analysed for the population age structure of Fabaeformiscandona gyirongensis. Ostracod valves are dominated by F. gyirongensis, with frequently occurring Ilyocypris sp. in the surface sediments. The distribution and abundance of ostracods are significantly correlated with the sampling depth and grain size, implying that hydrological conditions are the major controlling factor. The dominant species F. gyirongensis seems to prefer relatively deep and stable lacustrine conditions, while Ilyocypris sp. seems to prefer shallow conditions with rich submerged macrophytes and relatively coarse substrate in Dalongchi Lake. The spatial changes in the population age structure of F. gyirongensis match the different hydrodynamic regimes within the lake, with abundant early and middle instars in deeper waters and abundant middle and late instars in shallower waters, denoting that downslope transport of valves may be responsible for the spatial changes in the population structure. Our findings, together with previous works, indicate that downslope transport of instars and subsequent depth differentiation of the population structure of ostracods can occur for different species in both marine and lacustrine settings, which potentially leads to some biases based on the “in situ” inference of microfossils in palaeoenvironmental reconstruction. Hence, careful transport process assessment of fossil assemblages based on population age structure and other characteristics, such as the ratios of adults to juveniles and carapaces to valves, is a valuable prerequisite for palaeoenvironmental analysis.
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spelling doaj.art-0b19c0469a6443578457e17342418a132022-12-21T22:57:44ZengElsevierEcological Indicators1470-160X2021-11-01131108182Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossilsXin Mao0Xingqi Liu1Junfeng Li2Shengnan Feng3Gaolei Jiang4Linjing Liu5College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China; Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China; Key Laboratory of Quaternary Chronology and Hydrological-Environment Evolution, China Geological Survey, Shijiazhuang 050061, ChinaCollege of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China; Corresponding author at: College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China.Faculty of Resources and Environmental Science, Shijiazhuang University, Shijiazhuang 050035, ChinaCollege of Resource Environment and Tourism, Capital Normal University, Beijing 100048, ChinaInstitute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China; Key Laboratory of Quaternary Chronology and Hydrological-Environment Evolution, China Geological Survey, Shijiazhuang 050061, ChinaInstitute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China; Key Laboratory of Quaternary Chronology and Hydrological-Environment Evolution, China Geological Survey, Shijiazhuang 050061, ChinaIn palaeolimnology, microfossils play an important role as ecological indicators of lake history. A reliable interpretation of microfossil data requires a comprehensive understanding of transport processes as well as determining whether microfossil assemblages are representative of their living communities. The occurrence of transport in ostracod taphocoenoses can be identified from the population age structure of valves. In this study, 23 surface sediment samples from Dalongchi Lake, northwestern China, were analysed for species composition, and 16 were also analysed for the population age structure of Fabaeformiscandona gyirongensis. Ostracod valves are dominated by F. gyirongensis, with frequently occurring Ilyocypris sp. in the surface sediments. The distribution and abundance of ostracods are significantly correlated with the sampling depth and grain size, implying that hydrological conditions are the major controlling factor. The dominant species F. gyirongensis seems to prefer relatively deep and stable lacustrine conditions, while Ilyocypris sp. seems to prefer shallow conditions with rich submerged macrophytes and relatively coarse substrate in Dalongchi Lake. The spatial changes in the population age structure of F. gyirongensis match the different hydrodynamic regimes within the lake, with abundant early and middle instars in deeper waters and abundant middle and late instars in shallower waters, denoting that downslope transport of valves may be responsible for the spatial changes in the population structure. Our findings, together with previous works, indicate that downslope transport of instars and subsequent depth differentiation of the population structure of ostracods can occur for different species in both marine and lacustrine settings, which potentially leads to some biases based on the “in situ” inference of microfossils in palaeoenvironmental reconstruction. Hence, careful transport process assessment of fossil assemblages based on population age structure and other characteristics, such as the ratios of adults to juveniles and carapaces to valves, is a valuable prerequisite for palaeoenvironmental analysis.http://www.sciencedirect.com/science/article/pii/S1470160X21008475Dalongchi LakeSurface sedimentOstracodsPopulation structureTransport process
spellingShingle Xin Mao
Xingqi Liu
Junfeng Li
Shengnan Feng
Gaolei Jiang
Linjing Liu
Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils
Ecological Indicators
Dalongchi Lake
Surface sediment
Ostracods
Population structure
Transport process
title Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils
title_full Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils
title_fullStr Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils
title_full_unstemmed Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils
title_short Population age structure of ostracods in lake sediment and its implication for within-lake transport of microfossils
title_sort population age structure of ostracods in lake sediment and its implication for within lake transport of microfossils
topic Dalongchi Lake
Surface sediment
Ostracods
Population structure
Transport process
url http://www.sciencedirect.com/science/article/pii/S1470160X21008475
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