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Impacts of sea-level changes on mangroves from southeastern Brazil during the Holocene and Anthropocene using a multi-proxy approach

机译:海平变化对巴西东南巴西的红豆杉的影响,使用多功能方法

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摘要

Globally, mangroves are expected to move inland as sea-level rises. However, local characteristics mainly related to mangrove structure, geomorphology and coastal hydrodynamics may change the mangrove response to sea-level rise. The most useful evidence to support projections for the future likely comes from mangrove history reconstruction corresponding to past sea-level changes. This study characterized modern (1985-2018 CE) and past (6300 cal yr BP) mangrove dynamics according to sea-level changes along two estuarine valleys on the southeastern Brazilian coast to predict the mangrove response to sea-level rise by 2100. Relative Sea-Level (RSL) rise triggered changes from a tidal flat occupied by herbs, palms, tree/shrubs to a lagoon surrounded by mangroves between-6300 and-4230 cal yr BP. More recently, the RSL fall converted that lagoon into flats occupied by herbs, trees/shrubs, and palms on higher surfaces, and mangroves on lower flats during the mid-late Holocene. The last thousand years were characterized by a mangrove contraction between 390 and 77 cal yr BP, caused by a RSL fall. By contrast, mangrove expansion began at 77 cal yr BP (1873 CE) and continued after 1950 CE, migrating onto higher tidal flats previously occupied by herbs, palms, and trees/shrubs. Spatial-temporal analysis also indicated a mangrove invasion onto higher flats since 1985 CE. These trends are likely related to RSL rise since the end of the Little Ice Age and they intensified during recent decades, when the lower mangrove boundaries remained stable, and mangroves expanded to higher surfaces. Mangroves, confined between steep surfaces, will expand-22ha under the influence of a sea-level rise of 98 cm by 2100. However, an upstream mangrove migration by 2100 on low and extensive fluvial plains (-4030 ha) will depend mainly on the interaction between fluvial discharge/sea-level rise. (c) 2021 Elsevier B.V. All rights reserved.
机译:在全球范围内,预计红树林将随着海平面上升而移动内陆。然而,局部特征主要与红树林结构,地貌和沿海流体动力学相关,可能会改变红树林对海平面上升的反应。支持未来预测的最有用证据可能来自红树林历史重建,与过去的海平面变化相对应。本研究表征了现代(1985-2018 CE)和过去(< 6300 CAL YR BP)红树林动态,根据海上巴西海岸的两个河口山谷,以预测2100年的红树林的反应。相对海平面(RSL)上升从草药,棕榈树,树/灌木占据的潮汐平面触发的变化,以6300和-2230 Cal Yr BP之间的红树林包围的泻湖。最近,RSL堕落将该泻湖转化为草本,树木/灌木和棕榈树占领的平面,在较晚后期全新世期间在下层公寓上的红树林。剩下的千年来以390和77 Cal YR BP在RSL秋季引起的红树丛中的特征。相比之下,红树林扩张开始于77卢比(1873 CE),并在1950年后继续,迁移到以前由草药,棕榈树木和树木/灌木占据的更高潮流。自1985年以来,空间 - 时间分析还表明了红树林入侵到更高的单位。这些趋势可能与RSL上升以来,自冰河年龄的结束以来,当近几十年来,当较低的红树林界限保持稳定时,混合在较高的表面上。在陡峭的表面之间限制的红树林将在2100〜2100逐升98厘米的影响下扩大-22ha。然而,在低和广泛的河流平原(-4030公顷)上将上游红树林迁移到2100(-4030公顷)将主要取决于河流放电/海平面上升之间的相互作用。 (c)2021 elestvier b.v.保留所有权利。

著录项

  • 来源
    《Geomorphology》 |2021年第1期|107860.1-107860.21|共21页
  • 作者单位

    Fed Univ Para Grad Program Geol & Geochem Av Perimetral 2651 BR-66077530 Belem PA Brazil;

    Fed Univ Para Grad Program Geol & Geochem Av Perimetral 2651 BR-66077530 Belem PA Brazil|Univ Sao Paulo CENA 14C Lab Av Centenario 303 BR-13400000 Piracicaba SP Brazil;

    Fed Univ Para Grad Program Geol & Geochem Av Perimetral 2651 BR-66077530 Belem PA Brazil;

    Fed Univ Para Grad Program Geol & Geochem Av Perimetral 2651 BR-66077530 Belem PA Brazil;

    Univ Sao Paulo CENA 14C Lab Av Centenario 303 BR-13400000 Piracicaba SP Brazil;

    Univ Sao Paulo CENA 14C Lab Av Centenario 303 BR-13400000 Piracicaba SP Brazil;

    Fed Univ Para Grad Program Geol & Geochem Av Perimetral 2651 BR-66077530 Belem PA Brazil;

    Univ Sao Paulo CENA Stable Isotopes Lab Sao Paulo Brazil;

    Fluminense Fed Univ LAC UFF AMS Lab Phys Dept BR-24220900 Niteroi RJ Brazil;

    Phys Geog Lab UFES Vitoria ES Brazil;

    Louisiana State Univ Coll Coast & Environm Dept Oceanog & Coastal Sci Baton Rouge LA 70803 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; Guarapari; Mangrove; Photogrammetry; Pollen; Sea-level; Stable isotopes;

    机译:气候变化;Guarapari;红树林;摄影测量;花粉;海拔;稳定同位素;

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