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      Correction: Diversity and Above-Ground Biomass Patterns of Vascular Flora Induced by Flooding in the Drawdown Area of China's Three Gorges Reservoir

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          Abstract

          This study is a follow up to an earlier study reporting the results of a survey of vegetation carried out in 2009 which was published in the Polish Journal of Ecology (Reference 13 in the published article): Wang Q, Yuan XZ, Liu H, Zhang YW, Cheng ZL, et al. (2012) Effect of long-term winter flooding on the vascular flora in the drawdown area of the Three Georges Reservoir, China. Polish Journal of Ecology 60: 95–106. The current article reported a comparison of two consecutive years of data (2009 and 2010) using data from 12 of the 14 sites included in the original study; thus, some of the data generated by the 2009 survey and used in this analysis has been previously published. The relationship of the current study to the previous work was acknowledged in the paper; however, the authors would like to provide clarification of a number of instances in which previously published information/data were used in the article without an accompanying clear citation: - Information on sampling methods and the hydrological regime was similar to that reported in the Polish Journal of Ecology article. - The 2009 data on life forms (shown in Table 4) for 12 of the 14 original sampling sites were re-used from the previous study. - The 2009 data on patterns of life form and species richness along elevational gradient for 12 of the 14 original sampling sites were re-used from the previous study. In addition, the authors wish to clarify that Figs 1 and 3A were modified from the above article with permission from copyright holder Polish Journal of Ecology. The captions for Figs 1–3 and Table 2, Table 4 and Table 5 should be revised to read as follows: 10.1371/journal.pone.0147452.g001 Fig 1 Spatial distribution of the twelve sites sampled in 2010. The sites sampled in 2009 were mostly the same and were mapped previously [13]. The Three Gorges Reservoir Area is a combination of all the counties around the reservoir. Modified from [13] with permission from Polish Journal of Ecology. 10.1371/journal.pone.0147452.g002 Fig 2 Water level of the Three Gorges Reservoir between August 2006 and December 2010. Data updated from [13] to include July 2009 –Dec 2010. Data originate from the daily records of the Three Gorges Dam hydrology station (http://www.ctgpc.com.cn/index.php). The vertical arrows indicated the period for field sampling. 10.1371/journal.pone.0147452.g003 Fig 3 Life form percentage, species richness in plot (mean±SD), Shannon-Wiener Index (mean±SD) and above-ground biomass (mean±SD) of vegetation communities across the elevation zones in 2009 and 2010. Life form percentage was calculated by total recorded plant species date in each elevation zone. Different letters (a, b, c) above the boxes indicate significant differences for P<0.05. 3(a) is modified from [13] with permission from Polish Journal of Ecology. Life form percentage and species richness data for 2009 are taken from 12 of the 14 original sampling sites as previously reported in [13]. 10.1371/journal.pone.0147452.t001 Table 2 General environmental characteristics of the twelve sampling sites in the drawdown area of the Three Gorges Reservoir, as previously reported in [13]. Sampling site Location Longitude/latitude Slope Pre-dam land use S1 Taipingxi in Zigui county 30°51′N, 110°59′E 25° Dry land with a few woods S2 Xiaoxingtan in Xiling Gorge 30°56′N, 110°46′E 34° Shrubs and dry land S3 Xiangxi River Estuary 30°58′N, 110°45′E 15° Dry land S4 Luyou Hole in Wu Gorge 31°03′N, 109°54′E 48° Shrubs S5 Dachang in Wushan County 31°15′N, 109°49′E 20° Dry land S6 Baidicheng in Qutang Gorge 31°02′N, 109°34′E 25° Shrubs S7 Shuangjiang in Yunyang County 30°56′N, 108°41′E 30° paddy field S8 Baijia Stream in Kaixian County 31°08′N, 108°33′E 15° Rice paddy and dry land S9 Laotudi in Kaixian County 31°09′N, 108°34′E 10° Paddy field S10 Huanghua Island in Zhongxian County 30°19′N, 108°05′E 20° Paddy field S11 Dongxi Stream in Zhongxian County 30°16′N, 108°04′E 18° Paddy field S12 Baiyansi in Fuling County 29°43′N, 107°23′E 25° Dry land and village land 10.1371/journal.pone.0147452.t002 Table 4 Comparison of the absolute number and percentage of each life form category in the drawdown area before impoundment by the Three Gorges Dam and after impoundment in both 2009 and 2010. Data for 2009 are taken from 12 of the 14 sites as previously reported in [13]. Life form No. of sp. Percentage (%) 2009 2010 2009 2010 Phanerophytes 30 16 17.1 12.6 Chamaephytes 14 11 8.0 8.7 Hemicryptophytes 16 14 9.1 11.0 Cryptophytes 28 23 16.1 18.1 Therophytes 87 63 49.7 49.6 Total 175 127 100 100 10.1371/journal.pone.0147452.t003 Table 5 Comparison of total established sites number in twelve sampling sites of eight woody plant species in both 2009 and 2010. Data from 2009 survey for Vitex negundo L., Morus alba L., and Sapium sebiferumL. Roxb. as previously reported in [13]. Species 2009 2010 Vitex negundo L. 8 2 Morus alba L. 6 1 Sapium sebiferum L. Roxb. 6 2 Glochidion puberum L. Hutch. 5 1 Rhus chinensis Mill. 4 1 Melia azedarach L. 3 0 Pterocarya stenoptera DC. 3 1 Trema levigata Hand.-Mazz. 3 2

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          Diversity and Above-Ground Biomass Patterns of Vascular Flora Induced by Flooding in the Drawdown Area of China's Three Gorges Reservoir

          Hydrological alternation can dramatically influence riparian environments and shape riparian vegetation zonation. However, it was difficult to predict the status in the drawdown area of the Three Gorges Reservoir (TGR), because the hydrological regime created by the dam involves both short periods of summer flooding and long-term winter impoundment for half a year. In order to examine the effects of hydrological alternation on plant diversity and biomass in the drawdown area of TGR, twelve sites distributed along the length of the drawdown area of TGR were chosen to explore the lateral pattern of plant diversity and above-ground biomass at the ends of growing seasons in 2009 and 2010. We recorded 175 vascular plant species in 2009 and 127 in 2010, indicating that a significant loss of vascular flora in the drawdown area of TGR resulted from the new hydrological regimes. Cynodon dactylon and Cyperus rotundus had high tolerance to short periods of summer flooding and long-term winter flooding. Almost half of the remnant species were annuals. Species richness, Shannon-Wiener Index and above-ground biomass of vegetation exhibited an increasing pattern along the elevation gradient, being greater at higher elevations subjected to lower submergence stress. Plant diversity, above-ground biomass and species distribution were significantly influenced by the duration of submergence relative to elevation in both summer and previous winter. Several million tonnes of vegetation would be accumulated on the drawdown area of TGR in every summer and some adverse environmental problems may be introduced when it was submerged in winter. We conclude that vascular flora biodiversity in the drawdown area of TGR has dramatically declined after the impoundment to full capacity. The new hydrological condition, characterized by long-term winter flooding and short periods of summer flooding, determined vegetation biodiversity and above-ground biomass patterns along the elevation gradient in the drawdown area.
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            Journal
            PLoS One
            PLoS ONE
            plos
            plosone
            PLoS ONE
            Public Library of Science (San Francisco, CA USA )
            1932-6203
            19 January 2016
            2016
            : 11
            : 1
            : e0147452
            Article
            PONE-D-16-00488
            10.1371/journal.pone.0147452
            4718539
            26784902
            19063f30-cc86-4934-aa89-a1cfe920a8f5
            © 2016 Wang et al

            This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

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