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BIODIVERSITY OF SALINE AND BRACKISH MARSHES OF THE INDIAN RIVER LAGOON: HISTORIC AND CURRENT PATTERNS

机译:印度洋泻湖的盐渍和咸淡水沼泽的生物多样性:历史和当前格局

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摘要

The Indian River Lagoon (IRL) crosses a zone of climatic transition. Historically, marshes dominated saline and brackish environments in the north of the lagoon, while mangroves were dominant to the south. Periodic freezes limited mangrove distribution and abundance. A unique feature of most IRL marshes was seasonal and wind-driven tidal inundation rather than daily tidal fluctuations; near inlets, tidally influenced marshes occurred. Distribution of marsh communities was influenced by hydrology, salinity, soil characteristics, and fire, as well as periodic freezes. Major marsh community types included cabbage palm (Sabal palmetto) savanna, sand cordgrass (Spartina bakeri) marsh, black rush (Juncus roemerianus) marsh, saltgrass marsh (Distichlis spicata, Paspalum distichum), and mixed halophyte (Batis maritima, Salicornia virginica) marsh. Mud flats occupied significant areas. Black (Avicennia germinans) and white (Languncularia racemosa) mangroves occurred in some areas in open to dense stands associated with saltgrasses and mixed halophytes. Red mangroves (Rhizo-phora mangle) apparently occurred as scattered individuals fringing the lagoon. Many of these communities were marked by a few dominant species and relatively low within-community plant species diversity. The resulting landscape pattern was complex and diverse. Marshes of the Indian River Lagoon have been greatly modified since the 1940s. Impoundment or ditching for mosquito control has affected most areas. Much of the low marsh was replaced by open water or by extensive cattail {Typha cf. domingensis) marshes. Loss of connection with the uplands and changed hydrology probably reduced fire frequency and intensity in the high marshes, favoring invasion by wetland shrubs (Salix caroliniana, Myrica cerifera, Baccharis spp.) and the exotic Brazilian pepper (Schinus terebinthifolius). Other impacts to marshes include dredging and filling and nutrient enrichment. Dominant and characteristic plant species of these saline and brackish marshes are widespread throughout the Indian River Lagoon. Few rare plants are associated with Indian River Lagoon marshes. Despite significant modifications, marsh plant species have not been lost from the region, but community and landscape patterns have been greatly modified and ecosystem processes altered. Vertebrates dependent on these marshes have not all faired as well, as evidenced by the extinction of the Dusky Seaside Sparrow (Ammodramus maritimus nigrescens) that depended on marshes of the Indian River Lagoon and the St. Johns River.
机译:印度河泻湖(IRL)穿越气候过渡带。从历史上看,沼泽在泻湖北部占主导地位,盐碱和咸淡的环境中,而南部则占主导地位的是红树林。定期冻结会限制红树林的分布和丰度。大多数IRL沼泽的一个独特特征是季节性和风力驱动的潮汐淹没,而不是每日的潮汐波动。在入口附近,受潮汐影响的沼泽发生了。沼泽群落的分布受水文,盐度,土壤特征,火灾和定期冻害的影响。主要的沼泽群落类型包括白菜棕榈(Sabal palmetto)稀树草原,砂草(Spartina bakeri)沼泽,黑草(Juncus roemerianus)沼泽,盐草沼泽(Distichlis spicata,Paspalum distichum)和混合盐生植物(Batis maritima,Salicorsh virginica) 。泥滩占据了很大的面积。在与盐草和混合盐生植物相关的茂密林分中,一些地区出现了黑色(Avicennia菌属)和白色(Languncularia racemosa)红树林。红树林(Rhizo-phora mangle)显然是散布在泻湖边缘的个体。这些社区中的许多社区以少数优势种为标志,而社区内植物物种的多样性相对较低。由此产生的景观格局是复杂而多样的。自1940年代以来,印度河泻湖的沼泽得到了极大的改造。蓄水或沟渠控制蚊子影响了大多数地区。低洼沼泽地的大部分被开阔水域或大量香蒲所取代{Typha cf. domingensis)沼泽。失去与高地的联系以及水文状况的变化可能会降低高沼地的火灾频率和强度,有利于湿地灌木(Salix caroliniana,Myrica cerifera,Baccharis spp。)和外来的巴西胡椒(Schinus terebinthifolius)的入侵。对沼泽的其他影响包括疏and和填充以及养分富集。这些盐碱和咸淡沼泽的主要和特征性植物物种遍布整个印度河泻湖。很少有稀有植物与印度河泻湖沼泽相关。尽管进行了重大改动,但沼泽植物种类并未从该地区消失,但社区和景观格局已得到很大改变,生态系统过程也发生了变化。依赖于这些沼泽地的脊椎动物还不尽如人意,这证明了依靠印度河泻湖和圣约翰斯河沼泽地的暗夜麻雀(Ammodramus maritimus nigrescens)的灭绝。

著录项

  • 来源
    《Bulletin of Marine Science》 |1995年第1期|p.37-48|共12页
  • 作者

    Paul A. Schmalzer;

  • 作者单位

    Dynamac Corp. Mail Code DYN-2, NASA, Biomedical Operations and Research Office, Kennedy Space Center, Florida 32899;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋学;
  • 关键词

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