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Aggregated Clumps of Lithistid Sponges: A Singular Reef-Like Bathyal Habitat with Relevant Paleontological Connections

机译:蜡状海绵的聚集块:具有类似古生物学联系的奇异的礁石般的深海栖息地

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摘要

The advent of deep-sea exploration using video cameras has uncovered extensive sponge aggregations in virtually all oceans. Yet, a distinct type is herein reported from the Mediterranean: a monospecific reef-like formation built by the lithistid demosponge Leiodermatium pfeifferae. Erect, plate-like individuals (up to 80 cm) form bulky clumps, making up to 1.8 m high mounds (1.14 m on average) on the bottom, at a 760 m-deep seamount named SSS. The siliceous skeletal frameworks of the lithistids persist after sponge death, serving as a complex 3D substratum where new lithistids recruit, along with a varied fauna of other sessile and vagile organisms. The intricate aggregation of lithistid mounds functions as a “reef” formation, architecturally different from the archetypal "demosponge gardens" with disaggregating siliceous skeletons. Leiodermatium pfeifferae also occurred at two additional, close seamounts (EBJ and EBS), but, unlike at SSS, the isolated individuals never formed accretive clumps. The general oceanographic variables (temperature, salinity, dissolved nutrients, chlorophyll, and oxygen) revealed only minimal between-seamount differences, which cannot explain why sponge abundance at SSS is about two orders of magnitude higher than at EBJ or EBS. Large areas of the dense SSS aggregation were damaged, with detached and broken sponges and a few tangled fishing lines. Satellite vessel monitoring revealed low fishing activity around these seamounts. In contrast, international plans for gas and oil extraction at those locations raise serious concerns over the need for protecting urgently this unique, vulnerable habitat to avoid further alteration. Modern lithistids are a relict fauna from Jurassic and Cretaceous reefs and the roots of the very genus Leiodermatium can be traced back to those fossil formations. Therefore, understanding the causes behind the discovered lithistid aggregation is critical not only to its preservation, but also to elucidate how the extraordinary Mesozoic lithistid formations developed and functioned.
机译:使用摄像机进行深海勘探的到来,发现了几乎所有海洋中大量的海绵聚集体。然而,本文从地中海报道了一种独特的类型:由组蛋白的破骨海绵体(Leiodermatium pfeifferae)建立的单特异性礁石样构造。直立的板状个体(最大80厘米)形成大块,在一个深达760 m的海山SSS上,底部形成高达1.8 m的土丘(平均1.14 m)。海绵死亡后,类群的硅质骨骼骨架仍然存在,是一个复杂的3D基质,新的类群会聚集在那里,还有其他无柄和易变生物的动物群。混杂的石堆丘起着“礁石”的作用,在结构上不同于具有硅质骨架分解的原型“ Demosponge花园”。菲氏皮肤癣菌还发生在另外两个近海山(EBJ和EBS)上,但是与SSS不同,这些孤立的个体从未形成增生性团块。一般海洋学变量(温度,盐度,溶解的养分,叶绿素和氧气)显示出最小的海山间差异,这不能解释为什么SSS的海绵丰度比EBJ或EBS高约两个数量级。密集的SSS聚集体的大面积受到破坏,海绵脱落并破裂,钓鱼线有些缠结。卫星船只的监测表明,这些海山周围的捕鱼活动较少。相反,这些地区的国际天然气和石油开采计划引起了人们的严重关切,即迫切需要保护这一独特而脆弱的生境以避免进一步的改变。现代的组群动物是侏罗纪和白垩纪珊瑚礁的遗迹动物群,并且Leiodermatium属的根源可以追溯到这些化石的形成。因此,了解所发现的组蛋白聚集背后的原因不仅对它的保存至关重要,而且对于阐明异常的中生代组蛋白的发育和功能至关重要。

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