Solifluction meets vegetation: the role of biogeomorphic feedbacks for turf‐banked solifluction lobe development

机译：统一符合植被：草坪型血液菌叶发育的生物果状反馈的作用

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Abstract > Vegetation is an important factor influencing solifluction processes, while at the same time, solifluction processes and landforms influence species composition, fine‐scale distribution and corresponding ecosystem functioning. However, how feedbacks between plants and solifluction processes influence the development of turf‐banked solifluction lobes (TBLs) and their geomorphic and vegetation patterns is still poorly understood. We addressed this knowledge gap in a detailed biogeomorphic investigation in the Turtmann glacier foreland (Switzerland). Methods employed include geomorphic and vegetation mapping, terrain assessment with unmanned aerial vehicle (UAV) and temperature logging. Results were subsequently integrated with knowledge from previous geomorphic and ecologic studies into a conceptual model. Our results show that geomorphic and vegetation patterns at TBLs are closely linked through the lobe elements tread, risers and ridge. A conceptual four‐stage biogeomorphic model of TBL development with ecosystem engineering by the dwarf shrub <fc> <fi>Dryas octopetala</fi> </fc> as the dominant process can explain these interlinked patterns. Based on this model, we demonstrate that TBLs are biogeomorphic structures and follow a cyclic development, during which the role of their components for engineer and non‐engineer species changes. Our study presents the first biogeomorphic model of TBL development and highlights the applicability and necessity of biogeomorphic approaches and research in periglacial environments. Copyright ? 2016 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”>摘要</ title> >植被是影响局部流程的重要因素，虽然同时，塑性过程和地貌影响物种组成，细尺分布和相应的生态系统功能。然而，植物和求征过程之间的反馈如何影响草坪 - 银币血液裂隙（TBL）的发育及其地貌和植被模式仍然不明显。我们在Turtmann Glacier Foreland（瑞士）的详细生物质正式调查中解决了这一知识差距。采用的方法包括地貌和植被映射，与无人驾驶飞行器（UAV）和温度测井的地形评估。结果随后与以前的地貌和生态研究的知识集成到概念模型中。我们的研究结果表明，TBLS的地貌和植被模式通过瓣元素胎面，立管和脊紧密相关。 Dwarf灌木<FC> <FI> DryaS octopetala </ Fi> </ Fi> </ Fi> </ Fi> </ Fi> </ Fi>用生态系统工程的概念性四阶段生物果断模型。基于该模型，我们证明TBLS是生物果断结构并遵循循环开发，在此期间其组件为工程师和非工程师物种的作用变化。我们的研究介绍了TBL发展的第一个生物徽章模型，并突出了生物果断方法的适用性和必要性以及在悬垂环境中的研究。版权？ 2016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11期</span><b style="margin: 0 2px;">|</b><span>共13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=Eichel Jana&option=202" target="_blank" rel="nofollow">Eichel Jana;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Draebing Daniel&option=202" target="_blank" rel="nofollow">Draebing Daniel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Klingbeil Lasse&option=202" target="_blank" rel="nofollow">Klingbeil Lasse;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wieland Markus&option=202" target="_blank" rel="nofollow">Wieland Markus;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eling Christian&option=202" target="_blank" rel="nofollow">Eling Christian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmidtlein Sebastian&option=202" target="_blank" rel="nofollow">Schmidtlein Sebastian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kuhlmann Heiner&option=202" target="_blank" rel="nofollow">Kuhlmann Heiner;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dikau Richard&option=202" target="_blank" rel="nofollow">Dikau Richard;</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>Department of GeographyUniversity of BonnBonn Germany;</p> <p>Chair of Landslide ResearchTechnical University MunichMunich Germany;</p> <p>Institute of Geodesy and GeoinformationUniversity of BonnBonn Germany;</p> <p>Institute of Geodesy and GeoinformationUniversity of BonnBonn Germany;</p> <p>Institute of Geodesy and GeoinformationUniversity of BonnBonn Germany;</p> <p>Department of Geography and GeoecologyKarlsruhe Institute of TechnologyKarlsruhe Germany;</p> <p>Institute of Geodesy and GeoinformationUniversity of BonnBonn Germany;</p> <p>Department of GeographyUniversity of BonnBonn Germany;</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=biogeomorphology&option=203" rel="nofollow">biogeomorphology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=periglacial&option=203" rel="nofollow">periglacial;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ecosystem engineering&option=203" rel="nofollow">ecosystem engineering;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glacier foreland&option=203" rel="nofollow">glacier foreland;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=solifluction&option=203" rel="nofollow">solifluction;</a> </p> <div class="translation"> 机译：生物徽章;褶皱;生态系统工程;冰川前兰德;争夺; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023139090.html">Solifluction meets vegetation: the role of biogeomorphic feedbacks for turf‐banked solifluction lobe development</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eichel Jana&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Eichel Jana,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Draebing Daniel&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Draebing Daniel,</a> <a 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