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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Geo-hydromorphological assessment of Europe's southernmost blanket bogs
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Geo-hydromorphological assessment of Europe's southernmost blanket bogs

机译:欧洲最南端的毯子沼泽的地质水质形式评估

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摘要

Blanket bogs are a globally rare type of ombrotrophic peatland internationally recognized for long-term terrestrial carbon storage, the potential to serve as carbon sinks, habitat provision and for their palaeoenvironmental archive. This habitat is protected in the European Union under the Habitats Directive (92/43/EEC), but a number of blanket bogs located in the Cantabrian Mountains (northern Spain), representing the southernmost known edge-of-range for this habitat in Europe, are currently not recognized and are at increased threat of loss. Using climatic data, topography, aerial photography and peat depth surveys, this study has identified 10 new areas of blanket bog located between the administrative regions of Cantabria and Castilla y Leon. Peat depth data and topography were used to provide a detailed geomorphological description and hydromorphological classification (mesotope units) of these currently unrecognized areas of blanket bog. Maximum peat depth measured across the 10 sites ranged from 1.61 to 3.78 m, covering a total area of 18.6 ha of blanket bog (>40 cm peat depth). The volume of peat accumulated across the sites was determined to be more than 216 000 m(3)and is estimated to hold 19.89 +/- 3.51 kt C. Twenty-four individual hydrological mesotope units were described, indicating a diverse assemblage of blanket bogs in this region. The peatlands identified in this research extend the known limit of blanket bogs in Europe farther south than previously recorded and - combined with four other unprotected blanket bogs recently identified in the Cantabrian Mountains - these peatlands represent 10.5% of blanket bog currently recognized and protected in Spain. The range of anthropogenic pressures currently acting on peatlands in the Cantabrian Mountains indicates that without protection these important landforms and stored carbon may be lost. An urgent update of European peatland inventories is thus required to preserve these valuable carbon stores and potential carbon sinks. (c) 2020 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd
机译:毯子沼泽是全球罕见的令人抑制般的令人障碍泥潭,用于长期陆地碳储存,潜在的碳汇,栖息地提供和他们的古环境档案。该栖息地在栖息地指令下在欧盟(92/43 / EEC)下受到保护,但许多位于坎塔布山脉(北西班牙)的毯子沼泽,代表了欧洲这个栖息地的最南端,目前无法识别,并且正在增加损失威胁。本研究已经使用气候数据,地形,航拍和泥炭深度调查,确定了坎塔布里亚行政区和卡斯蒂略·莱昂的行政区之间的10个毯子沼泽地区。泥炭深度数据和地形用于提供这些目前无法识别的毯子沼泽区域的详细地貌描述和水样分类(Mesotope单位)。在10个地点测量的最大泥炭深度范围从1.61到3.78米,覆盖总面积为18.6公顷的毯子沼泽(> 40厘米的泥炭深度)。确定在该部位积聚的泥炭体积大于216000米(3),估计持有19.89 +/- 3.51 kt C. 24个单独的水文中分介剂单元,表明毯子沼泽的多样化组合在这个地区。本研究中确定的泥炭块延伸了欧洲的毯子沼泽的已知极限而不是以前记录的,并结合了坎塔布里亚山区最近确定的四个其他无保护的毯子沼泽 - 这些泥炭地代表了10.5%的毯子沼泽目前在西班牙公认和保护。 。目前在Cantabrian山脉泥炭地上作用的人为压力范围表明,没有保护这些重要地貌,储存的碳可能会丢失。因此需要紧急更新欧洲泥炭地库存来保护这些有价值的碳储存和潜在的碳汇。 (c)2020作者。 John Wiley&Sons Ltd发布的地球表面流程和地貌

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