The Greenland–Scotland Ridge in a Changing Ocean: Time to Act?

Marine Ecology Pub Date : 2024-08-08 DOI:10.1111/maec.12830
Christophe Pampoulie, Saskia Brix, H. Randhawa
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Abstract

The Greenland–Scotland Ridge is a submarine mountain that rises up to 500 m below the sea surface and extends from the east coast of Greenland to the continental shelf of Iceland and across the Faroe Islands to Scotland. The ridge not only separates deeper ocean basins on either side, that is, the North Atlantic and Arctic oceans, but also forms a geomorphological barrier between the cold arctic water masses of the Nordic Seas and the comparably contrastingly warmer water of the North Atlantic Ocean. It is therefore situated at a strategic geographical position in relation to the effect of climate change in the Arctic region. Both the Arctic and the Atlantic subpolar ecosystems are facing each other at the ridge, creating oceanic fronts in the Denmark Strait and in the Iceland–Faroe ridge alike. This ridge in the subarctic area forms the southern boundary of the North Atlantic Gateway to the Arctic Ocean, affecting exchanges of oceanic currents and of marine organisms between the two main ecosystems in the Nordic polar region. For example, the appearance of natural invasive species such as the Atlantic mackerel in this region mainly occurred along the ridge, with arrival through the Scotland–Faroe Islands mount with subsequent waves of colonization which eventually reached the southern tip of Greenland. With the increasing impacts of climate change, such natural colonization through the ridge is likely to happen more frequently and affect regional ecosystems. Yet, the human resources and the economy of the local nations on the ridge are rather limited compared to neighboring countries. With a total of less than half a million people inhabiting the area and a total ocean surface of circa 3 million km2 of continental shelf, Greenland, Iceland, the Faroe Islands, and Scotland will face critical challenges in the coming years with respect to biodiversity conservation and sustainable management of marine resources. Here is a summary of what we know, what we might expect, and an opening to potential discussions for the future of research in this region. The main objective of this paper is calling attention to much needed additional research effort on the marine environment around the Greenland–Scotland Ridge, instead of presenting a comprehensive overview of research in this area.
变化海洋中的格陵兰-苏格兰海脊:是时候采取行动了吗?
格陵兰-苏格兰海脊是一座海底山脉,在海面以下 500 米处隆起,从格陵兰东海岸延伸至冰岛大陆架,横跨法罗群岛至苏格兰。该山脊不仅将两侧较深的海洋盆地(即北大西洋和北冰洋)分隔开来,而且在北欧海域寒冷的北极水团和北大西洋相对温暖的海水之间形成了一道地貌屏障。因此,在北极地区气候变化的影响方面,它处于战略性的地理位置。北冰洋和大西洋的亚极地生态系统都在海脊对峙,在丹麦海峡和冰岛-法罗海脊都形成了海洋前沿。亚极地地区的这一海脊构成了北大西洋通往北冰洋的南部边界,影响着北欧极地地区两大生态系统之间洋流和海洋生物的交流。例如,大西洋鲭鱼等自然入侵物种在这一地区的出现主要是沿着海脊,通过苏格兰-法罗群岛山脉到达,随后的殖民浪潮最终到达格陵兰岛南端。随着气候变化的影响越来越大,这种通过海脊的自然殖民可能会更频繁地发生,并影响区域生态系统。然而,与邻国相比,海脊上当地国家的人力资源和经济实力相当有限。格陵兰岛、冰岛、法罗群岛和苏格兰的人口总数不到 50 万,大陆架总面积约为 300 万平方公里,在未来几年中,它们将在生物多样性保护和海洋资源可持续管理方面面临严峻挑战。本文概述了我们所知道的、我们可能期待的情况,并为这一地区未来的研究工作展开了可能的讨论。本文的主要目的是呼吁人们关注格陵兰-苏格兰海脊周围海洋环境亟需开展的更多研究工作,而不是对该地区的研究工作进行全面概述。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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