Translocation of Phytoliths Within Natural Soil Profiles in Northeast China

Phytoliths are a reliable paleovegetation proxy and have made an important contribution to paleoclimatic studies. However, little is known about the depositional processes affecting soil phytoliths, which limits their use for paleoclimate and paleovegetation reconstructions. Here, we present the res...

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Main Authors: Lidan Liu, Dehui Li, Dongmei Jie, Hongyan Liu, Guizai Gao, Nannan Li
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-10-01
Series:Frontiers in Plant Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fpls.2019.01254/full
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spelling doaj-0203bd80209f448d99053b093c125f872020-11-25T01:07:36ZengFrontiers Media S.A.Frontiers in Plant Science1664-462X2019-10-011010.3389/fpls.2019.01254471331Translocation of Phytoliths Within Natural Soil Profiles in Northeast ChinaLidan Liu0Dehui Li1Dehui Li2Dehui Li3Dongmei Jie4Dongmei Jie5Dongmei Jie6Hongyan Liu7Guizai Gao8Guizai Gao9Guizai Gao10Nannan Li11Nannan Li12Nannan Li13College of Resources and Environmental Science, Hunan Normal University, Changsha, ChinaInstitute for Peat and Mire Research, State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Northeast Normal University, Changchun, ChinaKey Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, Changchun, ChinaKey Laboratory of Vegetation Ecology, Ministry of Education, Changchun, ChinaInstitute for Peat and Mire Research, State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Northeast Normal University, Changchun, ChinaKey Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, Changchun, ChinaKey Laboratory of Vegetation Ecology, Ministry of Education, Changchun, ChinaResources Environment & Tourism, Anyang Normal University, Anyang, ChinaInstitute for Peat and Mire Research, State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Northeast Normal University, Changchun, ChinaKey Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, Changchun, ChinaKey Laboratory of Vegetation Ecology, Ministry of Education, Changchun, ChinaInstitute for Peat and Mire Research, State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Northeast Normal University, Changchun, ChinaKey Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, Changchun, ChinaKey Laboratory of Vegetation Ecology, Ministry of Education, Changchun, ChinaPhytoliths are a reliable paleovegetation proxy and have made an important contribution to paleoclimatic studies. However, little is known about the depositional processes affecting soil phytoliths, which limits their use for paleoclimate and paleovegetation reconstructions. Here, we present the results of a study of the vertical translocation characteristics of phytoliths in 40 natural soil profiles in Northeast China. The results show that phytolith concentration decreases within the humic horizon of the soil profiles and that ∼22% of the phytoliths are translocated below the surface of the studied soils. In addition, we find that the translocation rate of phytoliths varies markedly with phytolith type and that phytolith size and aspect ratio also have a significant effect. Phytoliths with length >30 μm and with aspect ratio >2 and those with length <20 μm and aspect ratio <2 are preferentially translocated compared to those with length >25 μm and aspect ratio <2. Our results demonstrate that differential translocation of phytoliths within soil profiles should be considered when using soil phytoliths for paleoclimate and paleovegetation reconstruction.https://www.frontiersin.org/article/10.3389/fpls.2019.01254/fullphytolithtransport characteristicspaleovegetationclimatic proxyNortheast China
collection DOAJ
language English
format Article
sources DOAJ
author Lidan Liu
Dehui Li
Dehui Li
Dehui Li
Dongmei Jie
Dongmei Jie
Dongmei Jie
Hongyan Liu
Guizai Gao
Guizai Gao
Guizai Gao
Nannan Li
Nannan Li
Nannan Li
spellingShingle Lidan Liu
Dehui Li
Dehui Li
Dehui Li
Dongmei Jie
Dongmei Jie
Dongmei Jie
Hongyan Liu
Guizai Gao
Guizai Gao
Guizai Gao
Nannan Li
Nannan Li
Nannan Li
Translocation of Phytoliths Within Natural Soil Profiles in Northeast China
Frontiers in Plant Science
phytolith
transport characteristics
paleovegetation
climatic proxy
Northeast China
author_facet Lidan Liu
Dehui Li
Dehui Li
Dehui Li
Dongmei Jie
Dongmei Jie
Dongmei Jie
Hongyan Liu
Guizai Gao
Guizai Gao
Guizai Gao
Nannan Li
Nannan Li
Nannan Li
author_sort Lidan Liu
title Translocation of Phytoliths Within Natural Soil Profiles in Northeast China
title_short Translocation of Phytoliths Within Natural Soil Profiles in Northeast China
title_full Translocation of Phytoliths Within Natural Soil Profiles in Northeast China
title_fullStr Translocation of Phytoliths Within Natural Soil Profiles in Northeast China
title_full_unstemmed Translocation of Phytoliths Within Natural Soil Profiles in Northeast China
title_sort translocation of phytoliths within natural soil profiles in northeast china
publisher Frontiers Media S.A.
series Frontiers in Plant Science
issn 1664-462X
publishDate 2019-10-01
description Phytoliths are a reliable paleovegetation proxy and have made an important contribution to paleoclimatic studies. However, little is known about the depositional processes affecting soil phytoliths, which limits their use for paleoclimate and paleovegetation reconstructions. Here, we present the results of a study of the vertical translocation characteristics of phytoliths in 40 natural soil profiles in Northeast China. The results show that phytolith concentration decreases within the humic horizon of the soil profiles and that ∼22% of the phytoliths are translocated below the surface of the studied soils. In addition, we find that the translocation rate of phytoliths varies markedly with phytolith type and that phytolith size and aspect ratio also have a significant effect. Phytoliths with length >30 μm and with aspect ratio >2 and those with length <20 μm and aspect ratio <2 are preferentially translocated compared to those with length >25 μm and aspect ratio <2. Our results demonstrate that differential translocation of phytoliths within soil profiles should be considered when using soil phytoliths for paleoclimate and paleovegetation reconstruction.
topic phytolith
transport characteristics
paleovegetation
climatic proxy
Northeast China
url https://www.frontiersin.org/article/10.3389/fpls.2019.01254/full
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