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Deep-sea calcareous rhodophycophyta communities in the levantine sea

机译:黎凡特海的深海钙质红藻藻类群落

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摘要

This study is based on materials from two cruises of r/v "Vityaz" : N 24 (1992) and N 27 (1993). In total 13 qualitative samples were collected at 6 stations on southern syrian shelf (depth 25-90 metres) (Figure 1) by means of trawling (Seegsby trawl) and dregging (grabb "Ocean-0,1") (Table 1). The community discovered there reminds the "Lithophyllum trotoir", "Trotoir a Tenarea" or "coralligenous bank" [3], well known for the Western Mediterranean. J.M.Peres [3] mentioned the same structures in the Eastern Mediterranean "covering very large areas - on thousands of square metres" (p. 500). The square of discovered by our expeditions "coralligenous meadow" is about some tens of square kilometres. Such formation is being described fro the first time. The second pecularity of this biocenosis is its location above silty substratum. The thickness of "coralligenous" layer is no more than 10 cm.
机译:这项研究基于r / v“ Vityaz”两次巡游的资料:N 24(1992)和N 27(1993)。通过拖网(Seegsby拖网)和撒水(抓斗“ Ocean-0,1”)(表1)在南部叙利亚架子(深度25-90米)(图1)的6个站点上总共收集了13个定性样品。那里发现的社区让人想起“ Lithophyllum trotoir”,“ Trenair a Tenarea”或“ coralligenous bank” [3],这在西地中海地区众所周知。佩雷斯(J.M. Peres)[3]提到了东地中海的“相同结构”,“面积非常大-数千平方米”(第500页)。我们的探险队发现的“珊瑚草甸”的平方大约是几十平方公里。这种形成是第一次被描述。这种生物污染的第二个特点是它位于粉质基质之上。 “珊瑚质”层的厚度不超过10厘米。

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