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Coralligenous habitat in the northern Adriatic Sea: an overview

机译:亚得里亚海北部的珊瑚生境:概述

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The rocky outcrops irregularly scattered in the sandy-muddy sea bed of the Northern Adriatic, formed by a base rock and a superimposed concretion of vegetal and animal organisms, are considered an infralittoral coralligenous habitat, according to the most recent definition. In the last four decades, research has mainly concentrated on their geology because of the question of the origin of the base rock - very similar to beachrock - which has only recently been attributed to sedimentary cementation induced by methane seeps. Studies on their macrobenthic assemblages have also been published recently, but true comparisons among them are difficult because they mostly refer only to a few selected phyla or to short-term observations. Very few papers deal with the whole of the animal and plant communities, including all taxonomic groups and the most important environmental variables. On the basis of the literature data concerning several outcrops in the Gulf of Venice, we suggest that the Adriatic reefs differ slightly from the classic deeper coralligenous assemblages around the Mediterranean coast because they have smaller concretions of algae builders. We also suggest that the Northern Adriatic coralligenous reefs are younger than the other reefs occurring in the Mediterranean Sea.
机译:根据最新定义,不规则散布在北亚得里亚海的沙泥海床中的岩石露头,由基岩和植物和动物有机体的叠加固结形成,被认为是沿陆珊瑚生境。在过去的四十年中,由于基本岩石的起源(与海滩岩石非常相似)的问题,研究主要集中在它们的地质上,直到最近才将其归因于甲烷渗漏引起的沉积胶结作用。关于它们的大型底栖动物组合的研究最近也已经发表,但是它们之间的真正比较是困难的,因为它们主要只涉及少数几个门或短期观察到的东西。很少有论文涉及整个动植物群落,包括所有生物分类群和最重要的环境变量。根据有关威尼斯湾几处露头的文献数据,我们建议亚得里亚礁与地中海沿岸的经典深层珊瑚群落略有不同,因为它们的藻类建造者较小。我们还建议,北部亚得里亚珊瑚礁比地中海其他珊瑚礁年轻。

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