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首页> 外文期刊>Marine Biodiversity >Deep-sea decapods sampled or observed with a manned submersible at the Rio Grande Rise (SW Atlantic), including the first record of four species from this region
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Deep-sea decapods sampled or observed with a manned submersible at the Rio Grande Rise (SW Atlantic), including the first record of four species from this region

机译:在RIO Grande崛起(SW Atlantic)的载人潜水中采样或观察到深海脱涂,包括来自该地区的四种物种的第一次记录

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摘要

The Rio Grande Rise (RGR) is a volcanic topographic structure of the Southwest Atlantic basin that rises over 3000 m from the seafloor and is located half way between the Brazilian continental margin (similar to 30A degrees S latitude) and the Mid-Atlantic Ridge. Previous records of decapods at the RGR are uncertain or non-existent. The observations and material examined here were collected by the manned submersible Shinkai 6500 during two dives to the plateau of the RGR main topographic feature, known as Alpha. Additional records were determined by analysing high-definition photos and videos obtained by the Shinkai 6500. Five species of deep-sea decapods were found: a Solenoceridae, Hymenopenaeus debilis Smith, 1882 previously sampled at the Brazilian slope; a Nematocarcinidae, Nematocarcinus parvus Burukovsky, 2000 previously unknown from the Atlantic Ocean; a Parapaguridae, Strobopagurus gracilipes (Milne-Edwards, 1891); a rare Palinuridae, Projasus parkeri (Stebbing, 1902); and the brachyuran Chaceon sanctaehelenae Manning & Holthuis, 1989 that were never sampled in the western Atlantic Ocean. The results show that the RGR decapod fauna is rare, unknown and, in its great majority, distinct, at the species level, from that found at the South American slope. At the genus and family levels, however, we can observe similarities between the RGR decapod fauna and that recorded on the South American slope. Unique exploration initiatives such as this can improve significantly the knowledge on western Atlantic deep-sea biodiversity and contribute to the understanding of deep-sea biogeography.
机译:Rio Grande崛起(RGR)是西南大西洋盆地的火山地形结构,距离海底超过3000米,位于巴西大陆边缘(类似于30A的纬度)和大西洋中部山脊之间的一半。在RGR处的先前记录的脱盖特是不确定或不存在的。这里检查的观察和材料在两种潜水期间被载人潜水的Shinkai 6500收集到RGR主要地形特征的高原,称为alpha。通过分析由Shinkai 6500获得的高清照片和视频分析了另外的记录。发现了五种深海褥疮:Solenoceridae,Hymenopenaeus debilis Smith,1882年以前在巴西坡上抽样; Nematocarcinidae,Nematocarcinus Parvus Burukovsky,2000年以前从大西洋未知; Parapaguridae,Strobopagurus Gracilipes(Milne-Edwards,1891);罕见的Palinuridae,Projasus Parkeri(Stebbing,1902);和Brachyuran Chaceon Sanctaehelenae Manning& Holthuis,1989年从未在西部大西洋中抽样过。结果表明,RGR Decapod Fauna是罕见的,未知的,并且在它的大多数情况下,在物种水平上,从南美坡上发现。然而,在Genus和家庭层面,我们可以观察RGR Decapod Fauna与南美坡度的相似之处。独特的勘探举措,如这可以大大提高西部大西洋深海生物多样性的知识,并有助于对深海生物地理学的理解。

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