量化芬兰波罗的海群岛海的海底地质多样性

IF 2 4区 地球科学 Q1 GEOLOGY
A. Kaskela, A. Kotilainen
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引用次数: 0

摘要

本研究调查了波罗的海北部群岛海的地质多样性,重点是地质特征及其空间分布。通过调整以往波罗的海研究中使用的方法,我们对地质数据集(包括基岩类型、海底底质和海底结构)进行了空间分析。基岩和底质数据可免费获取,而海底结构则是根据水深测量数据建立的模型。使用地质多样性指数对地质多样性进行量化,该指数考虑了物理要素的多样性、粗糙度和单元面积。分析结果表明,群岛海的海底环境多种多样,整个研究区域的地质多样性各不相同。造成地质多样性的重要特征包括基岩断裂和断层带以及大型末碛岩层。在芬兰的陆地地区也观察到类似的模式。分析还发现了群岛分区与地质多样性之间的关系,开阔海域的地质多样性比群岛中部和内部的地质多样性更为均匀。这项研究正式确认了群岛海海底的复杂性,并强调了了解塑造该地区的地质过程的重要性。研究结果可为海洋空间规划和可持续资源管理提供参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Quantifying seabed geodiversity of the Archipelago Sea, Baltic Sea, Finland
This study investigated the geodiversity of the Archipelago Sea in the northern Baltic Sea, focusing on geological features and their spatial distribution. By adapting methods used in previous Baltic Sea studies, we conducted spatial analyses of geological data sets including bedrock type, seabed substrates and seabed structures. Bedrock and substrate data were freely available, while seabed structures were modelled from bathymetry data. Geodiversity was quantified using a geodiversity index, which considers the variety of physical elements, roughness and area of the unit. The analyses revealed a diverse seabed environment in the Archipelago Sea with varying geodiversity throughout the study area. Significant features contributing to geodiversity included bedrock fracture and fault zones and large end-moraine formations. Similar patterns have been observed in terrestrial areas of Finland. The analyses also detected relations between archipelago zonation and geodiversity with areas of open sea more homogeneous than the middle and inner archipelago. This study formally recognises the complexity of the seabed in the Archipelago Sea and highlights the importance of understanding the geological processes shaping the region. The results can inform maritime spatial planning and sustainable resource management.
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来源期刊
Geus Bulletin
Geus Bulletin GEOLOGY-
CiteScore
2.80
自引率
17.60%
发文量
8
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