Late Holocene mangrove dynamics dominated by autogenic processes

机译：全新的红树红树林动态由自动过程主导

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Abstract > Generally, palaeoenvironmental interpretations consider only allogenic processes, when autogenic factors may have a strong influence on proxies of stratigraphic sequences. For instance, the Holocene history of the vegetation along the southern littoral of the State of Bahia in north‐eastern Brazil is characterized by mangrove dynamics controlled by allogenic processes. However, over smaller timescales (~700?years), autogenic processes may have controlled vegetation dynamics and hence observed pollen distribution. This work proposes tidal channel dynamics as one of the main cause for changes in pollen assemblage along the studied stratigraphic profiles during the last centuries, based on sedimentology, pollen and elemental analysis (δ 13 C, δ 15 N and C/N) and radiocarbon dating of sedimentary organic matter from two cores sampled from an abandoned meander and a tidal flat at the mouth of the Jucuru?u River. One core was sampled from a mangrove formed during the past ~550?cal yr <sc>bp</sc> . Another core recorded sediments in a várzea forest (swamp seasonally and permanently inundated by freshwater) located ~2.7?km from the current shoreline, which displayed a maximum age of ~680?cal yr <sc>bp</sc> . Two facies associations were identified: tidal channel (A) and tidal flat/oxbow lake (B). This work proposes allogenic processes as the main driving forces controlling the wetlands dynamics at the studied site during the Holocene. However, our data also reveal that part of the changes in vegetation over the last ~700?years reflect tidal channels and tidal flats development, which represent autogenic processes. The change in timescale analysis from the Holocene to recent centuries may have weakened the influence of allogenic factors. However, this needs interpretation with reference to the spatial scale of the depositional environment as the larger the depositional system analyzed, the stronger the influence of autogenic processes on stratigraphic sequences over longer timescales. Copyright ? 2017 John Wiley & Sons, Ltd. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><abstract xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”> <title type =“main”>抽象</ title> >一般来说，古环境解释只考虑同种异体过程，当自动因素可能对地层序列的代理产生强烈影响时。例如，沿巴西东北北南南方南方南方南部南方的全新世历史的特点是由同种异体过程控制的红树林动态。然而，在较小的时间尺度（〜700岁）上，自动过程可能具有受控植被动态，因此观察到的花粉分布。这项工作提出了潮汐通道动力学作为过去几个世纪在过去几个世纪沿着研究的地层概况变化的主要原因之一，基于沉积学，花粉和元素分析（δ 13 </ sup> c，δ<sup > 15 </ sup> n和c / n）和来自两个核心的沉积有机物的沉积有机物的radiocarbon约会，从废弃的曲折和jucuru口处采样的潮汐平，u河。在过去〜550？Cal Yr <sc> bp </ sc>中，从一个组成的红树林中取样了一个核心。另一个核心记录的沉积物在várzea</ i>森林（沼泽季节性和永久性的淡水中淹没），位于当前海岸线的〜2.7 km，它显示出最大年龄〜680？cal yr <sc> bp < / sc>。鉴定了两个相关联：潮气通道（A）和潮汐平/牛湖（B）。这项工作提出了同种异体过程作为在全新世期间控制研究现场的湿地动态的主要驱动力。然而，我们的数据还揭示了植被变化的一部分在过去700岁以下的植被中反映了潮汐渠道和潮汐平面开发，这代表了自动过程。从全新世到几个世纪的时间尺度分析的变化可能削弱了同种异体因素的影响。然而，这种需要解释沉积环境的空间量表，因为分析的沉积系统越大，容量过程对层次序列比较长时间的分层序列的影响越强。版权？ 2017年John Wiley＆amp; SONS，LTD。</ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2017年第13期</span><b style="margin: 0 2px;">|</b><span>共11页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moraes Caio A.&option=202" target="_blank" rel="nofollow">Moraes Caio A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fontes Neuza A.&option=202" target="_blank" rel="nofollow">Fontes Neuza A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cohen Marcelo C.L.&option=202" target="_blank" rel="nofollow">Cohen Marcelo C.L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fran?a Marlon Carlos&option=202" target="_blank" rel="nofollow">Fran?a Marlon Carlos;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pessenda Luiz C.R.&option=202" target="_blank" rel="nofollow">Pessenda Luiz C.R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rossetti Dilce F.&option=202" target="_blank" rel="nofollow">Rossetti Dilce F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Francisquini Mariah I.&option=202" target="_blank" rel="nofollow">Francisquini Mariah I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bendassolli José A.&option=202" target="_blank" rel="nofollow">Bendassolli José A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Macario Kita&option=202" target="_blank" rel="nofollow">Macario Kita;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Graduate Program of Geology and GeochemistryFederal University of ParáBelém Brazil;</p> <p>Graduate Program of Geology and GeochemistryFederal University of ParáBelém Brazil;</p> <p>Graduate Program of Geology and GeochemistryFederal University of ParáBelém Brazil;</p> <p>Federal Institute of ParáBelém Brazil;</p> <p>CENA/ 14 C Laboratory University of S?o PauloS?o Paulo Brazil;</p> <p>National Space Research Institute (INPE)S?o José dos CamposBrazil;</p> <p>CENA/ 14 C Laboratory University of S?o PauloS?o Paulo Brazil;</p> <p>CENA/Stable Isotopes LaboratoryUniversity of S?o PauloPiracicaba S?o Paulo;</p> <p>Physics DepartmentLAC‐UFF AMS Laboratory‐Fluminense Federal UniversityRio de Janeiro Brazil;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=C and N isotopes&option=203" rel="nofollow">C and N isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=climate&option=203" rel="nofollow">climate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holocene&option=203" rel="nofollow">Holocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=palynology&option=203" rel="nofollow">palynology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=relative sea level&option=203" rel="nofollow">relative sea level;</a> </p> <div class="translation"> 机译：C和N同位素;气候;全新世;椎间囊学;相对海平面; 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target="_blank" rel="nofollow" class="tuijian_authcolor"> . 林业科学 </a> </span> <span> . 2013</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-xiamen-university-natural-science_thesis/0201248485422.html">红树林凋落叶自然分解过程中土壤微生物的数量动态</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=庄铁城&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 庄铁城</a> <span> <a href="/journal-cn-4552/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 厦门大学学报（自然科学版） </a> </span> <span> . 1993</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201296904948.html">晚全新世淇澳岛红树林有孔虫记录与古环境意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈慧娴&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈慧娴</a> <a 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PROCESSORS, SUCH AS A CPU, AND A RELATED COMPUTER READABLE MEDIUM.</a> <b>[P]</b> . <span> 外国专利：  EP3036652A1 </span> <span> . 2016-06-29</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：计算平台，可重构硬件设备以及用于在可动态重构硬件设备上同时执行过程的方法（例如FPGA）以及指令集处理器（例如CPU）以及相关的计算机可读介质。 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023139095','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: 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