Gunnar Gad 40th European Marine Biology Symposium AG Zoosystematik und Morphologie Carl von Ossietzky University 26111 Oldenburg, Germany e-mail: gunnar.gad @mail.uni-oldenburg.de Vienna, 21-25 August 2005 Special thematic session on Seamounts and abrupt deep Topographies The Draconematidae (Nematoda) fauna of the plateau of the Great Meteor Seamount The examination of the Draconematidae revealed information on: (1) distribution and abundance of Draconematidae on the seamount and the surrounding deep sea (2) important clues regarding their taxonomy and phylogeny (3) zoogeography and possible origin of the species colonizing the plateau The occurrence of a diverse fauna of Draconematidae on the Great Meteor Seamount indicates that their distribution in oceanic habitats is more widespread than previously assumed. Example 1: A new species of the genus Tenuidraconema have been found. This is the first species of this genus reported from the Atlantic. Around the same time a Belgium colleague (Marten Raes, in press) discovered another congener living on North Atlantic cold-water corals. These deepsea coral reefs are assumed to be one of the locations in the North Atlantic from which the elongate, surface-dwelling Draconematidae may have managed to colonize the plateau. 50 μm Example 3: The four new Dracograllus-species as interstitial species inhabit the coarse calcareous sand of the plateau. The examination of them indicates the way in which this genus urgently needs to be revised, because within Dracograllus there are three species-groups which can clearly be delineated whereas one species-group remains heterogeneous. Furthermore, the next congeners of this species are known from the Mediterranean Sea. In the case of the stout interstitial Draconematidae, this is the most likely location from which a faunal exchange with the plateau may have taken place a slight fauna exchange between both localities. The Great Meteor Seamount is one of the largest of the 810 known seamounts of the North Atlantic and rises from a depth of 4,500 m up to 287 m below the surface of the sea. Its summit is a flat oval plateau of roughly 1,465 km2 size. The GMS is an old volcano with an age of 40-50 Mio. years and part of the Atlantis-Meteor-Seamount-Complex in the Iberian Basin. The distance to the nearest coast is about 1,600 km. The sediment covering the plateau of the GMS is biogenic coarse calcareous sand which has been proven to harbour an astonishingly diverse interstitial meiofauna. The inventory of the meiofauna was done during the SEMEC (Seamount Ecology) expedition to the GMS in 1998. Twenty major taxa of meiofauna were discovered including Draconematidae (Nematoda). The Draconematidae were chosen among others for this study because of their complex and specialised external morphology related to their mode of locomotion and the habitat they inhabit. At present, there are 80 known species of Draconematidae. The majority of species has been reported form the Indo-Pacific region, but distribution data of single species are still rare. The examined samples yielded 14 species of Draconematidae, 12 of them presumably new to science and representing nine genera. Four monotypic genera, known so far only from their type localities, are represented by new species on the plateau. The most abundant group on the plateau is constituted by the 4 interstitial species, followed by 8 surface-dwelling species. Only a few specimens of the 2 demersally dwelling species have been found on the plateau and the surrounding deep-sea bottom as well. There are four possible areas from which the Draconematidae may have managed to colonized the plateau of the GMS: (1) Deep-sea reefs of cold-water corals (see example 1) (2) Shallow water habitats of the North Atlantic (see example 2) (3) Coast of the Mediterranean Sea (see example 3) (4) Soft bottoms of the surrounding deep sea (see example 4) Example 2: Three new Prochaetosoma-species have been discovered inhabiting the plateau, probably as an endemic group. Remarkably, these species are easily distinguished by female features. They were found separately in different areas on the plateau with minor overlaps in their distribution. The next congeners of these species are found in shallow water habitats of the North Atlantic. Example 4: A new Cephalochaetosoma-species and another new species which, among others, is currently being described as a characteristic representative of a genus of deep-sea Draconematidae. These demersally dwelling species live on soft bottoms and have been found recently in several other deep-sea localities across the Atlantic. Cephalochaetosoma-species and representatives of this new genus have so far only been reported from the deep sea of the Pacific. Both species were found in low abundances on the plateau as well as in the surrounding deep sea, which indicates a slight fauna exchange between both localities.
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