长江中下游干流江豚岸线栖息地质量评估长江中下游干流江豚岸线栖息地质量评估

章晋秀, 陈懋, 韩祎, 雷珮玉, 王克雄, 梅志刚, 王丁

章晋秀, 陈懋, 韩祎, 雷珮玉, 王克雄, 梅志刚, 王丁. 长江中下游干流江豚岸线栖息地质量评估——长江中下游干流江豚岸线栖息地质量评估[J]. 水生生物学报, 2019, 43(S1): 56-61. DOI: 10.7541/2019.167
引用本文: 章晋秀, 陈懋, 韩祎, 雷珮玉, 王克雄, 梅志刚, 王丁. 长江中下游干流江豚岸线栖息地质量评估——长江中下游干流江豚岸线栖息地质量评估[J]. 水生生物学报, 2019, 43(S1): 56-61. DOI: 10.7541/2019.167
ZHANG Jin-Xiu, CHEN Mao, HAN Yi, LEI Pei-Yu, WANG Ke-Xiong, MEI Zhi-Gang, WANG Ding. RIVER BANK HABITAT ASSESSMENT OF THE YANGTZE FINLESS PORPOISE IN THE MAIN STEM OF MIDDLE-LOWER YANGTZE RIVER[J]. ACTA HYDROBIOLOGICA SINICA, 2019, 43(S1): 56-61. DOI: 10.7541/2019.167
Citation: ZHANG Jin-Xiu, CHEN Mao, HAN Yi, LEI Pei-Yu, WANG Ke-Xiong, MEI Zhi-Gang, WANG Ding. RIVER BANK HABITAT ASSESSMENT OF THE YANGTZE FINLESS PORPOISE IN THE MAIN STEM OF MIDDLE-LOWER YANGTZE RIVER[J]. ACTA HYDROBIOLOGICA SINICA, 2019, 43(S1): 56-61. DOI: 10.7541/2019.167

长江中下游干流江豚岸线栖息地质量评估——长江中下游干流江豚岸线栖息地质量评估

基金项目: 国家自然科学基金(31430080和31500456); “支撑长江经济带可持续发展的生态环境保护战略对策研究”资助
详细信息
    作者简介:

    章晋秀(1995—), 女, 安徽池州人; 硕士; 主要研究方向为鲸类保护生物学。E-mail: zhangjx@ihb.ac.cn

    通信作者:

    梅志刚(1986—), 主要研究方向为鲸类保护生物学。E-mail: meizhigang@ihb.ac.cn

  • 中图分类号: Q958.1

RIVER BANK HABITAT ASSESSMENT OF THE YANGTZE FINLESS PORPOISE IN THE MAIN STEM OF MIDDLE-LOWER YANGTZE RIVER

Funds: Supported by the National Natural Science Foundation of China (31430080, 31500456); Strategic Countermeasures of Ecological and Environmental Protection in Supporting Sustainable Development of the Yangtze Economic Belt
    Corresponding author:
  • 摘要: 栖息地环境质量直接影响长江江豚的种群数量与分布, 但当前长江中下游全尺度的江豚栖息地质量状况尚不清楚。研究于2017年11月10日至12月17日“2017年长江江豚生态科学考察”期间, 使用相机拍照采样的方法, 开展了长江中下游干流宜昌至上海江段江豚岸线栖息地质量现状调查。一共采集了794个有效岸线样点, 观察到江豚318次631头次。卡方拟合优度检验结果显示, 江豚在自然岸线的观测频数占比显著性高于其期望频数占比(χ2=68.99, P<0.001), 而在半自然岸线和固化岸线中结果却相反(χ2=39.26, P<0.001; χ2=12.15, P<0.001), 自然岸线是江豚偏好分布的栖息地类型。同时调查表明长江中下游干流自然岸线受到严重破坏, 半自然岸线和固化岸线占比达45.47%。此外, 岸线栖息地破碎化显著, 自然岸线的区域中间都间杂了半固化的或者完全固化的岸线, 这可能是导致长江干流江豚破碎化分布的主要原因。当前长江中下游干流岸线栖息地质量衰退与破碎化现象十分显著, 是江豚生存的重要威胁, 建议实施硬化岸线的自然恢复和重建破碎化岸线的连通性。
    Abstract: Habitat quality can directly affect population abundance and distribution of the Yangtze finless porpoise. This study investigated habitat status of both south and north banks of the main stem of the Yangtze River by taking high-resolution digital photos systematically during the 2017 Yangtze Freshwater Dolphin Expedition from 10th November to 17th December, 2017. The survey area covered the entire middle and lower reaches of the Yangtze River from Yichang to Shanghai (1669 km in length) and a total of 794 photo samples were collected. We recorded 318 sightings with 631 individuals of the Yangtze finless porpoise. The Chi-squared goodness of fit test revealed that proportions of observed frequency are significantly higher than the expected frequency in natural river banks (χ2=69.81, P<0.001). Whereas the result is opposite in the semi-natural and solidified river banks (χ2=39.26, P<0.001; χ2=12.15, P<0.001), indicating that the natural river banks were the preferred habitat of the Yangtze finless porpoise. The length of the semi-natural river and solidified banks accounted for 45.47% of the total length of the river bank, which intermingled with the patches of the natural river banks, demonstrating that the natural habitat was severely degraded and highly fragmented to impact the distribution of the Yangtze finless porpoise. Our study suggested that habitat degradation and fragmentation pose a significant threat to the survival of the Yangtze finless porpoise. Future conservation research and practice should focus on habitat restoration of the solidified river banks to reestablish and enhance habitat connectivity.
  • 图  1   不同岸线类型占比

    Figure  1.   Proportions of different types of the river bank

    图  2   长江中下游干流岸线环境现状

    Figure  2.   The river bank status of the main stem of the middle and lower reaches of the Yangtze River

    图  3   三种岸线类型中江豚目击的观测频数分布与期望频数分布(误差条表示各观测频数占比的95%置信区间)

    Figure  3.   Observed and expected frequent distribution of individuals in three river bank types (Error bars indicate 95% confidence intervals for each observed frequencies proportion)

    表  1   岸线拍摄影像判读指标及标准

    Table  1   Indicators and criteria for river bank images

    岸线类型Type of river banks判读标准Criteria
    自然泥质或沙质岸线Muddy or sandy river bank迎水坡面为裸露的洲滩, 自然长草, 底质为泥质或者沙质Riverside slope is covered by plants and the substrate is muddy or sandy
    自然岩石质岸线Rocky river bank迎水坡面为岩石质, 少量有自然长草Riverside slope is covered by rocks and sporadic plants
    自然岸线+抛石护坡Natural river bank and riprapping revetment迎水坡面堤脚用干砌块石、浆砌块石或浆砌预制块进行加固, 上半部分自然长草Lower parts of the riverside slope of the levee are reinforced with riprap and upper parts remains natural
    自然岸线+水泥护坡Natural river bank and concrete revetment迎水坡面堤脚用水泥混凝土硬化加固, 上半部分自然长草Lower parts of the riverside slope of the levee are reinforced with concrete and upper part remains natural
    水泥护坡Concrete revetment迎水坡面全部被水泥混凝土硬化加固Riverside slope is reinforced with concrete
    抛石护坡Riprapping revetment迎水坡面全部被干砌块石、浆砌块石或浆砌预制块进行加固Riverside slope is reinforced with riprap
    水泥+抛石护坡Concrete and riprapping revetment迎水坡面一部分用混凝土加固, 另一部分用干砌块石、浆砌块石或浆砌预制块进行加固Riverside slope is partially reinforced with concrete and partially reinforced with riprap
    下载: 导出CSV

    表  2   长江中下游干流不同区域岸线现状

    Table  2   Length of differently types of river banks in the three sections of the middle and lower reachesof the Yangtze River

    区域Area北岸岸线长度Length of the north river bank (km)南岸岸线长度Length of the south river bank (km)
    自然Natural半自然Semi-natural固化Solidified自然Natural半自然Semi-natural固化Solidified
    宜昌-鄂州Yichang-Ezhou382148168308199191
    鄂州-华阳Ezhou-Huayang142 23 44138 3041
    华阳-上海Huayang-Shanghai322103315411 54275
    下载: 导出CSV
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出版历程
  • 收稿日期:  2018-10-15
  • 修回日期:  2019-06-02
  • 网络出版日期:  2019-06-27
  • 发布日期:  2019-11-30

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