Mollusc species richness and abundance from shelf to abyssal depths in the Ross Sea (Antarctica): the importance of fine-mesh-towed gears and implications for future sampling

In polar areas, where benthic sampling is constrained by a series of limitations imposed by climate and logistic challenges, knowledge about the key elements required to plan a successful survey is fundamental. During the International Polar Year (IPY, 2007/2008), under the Census of Antarctic Marine Life (CAML), new sampling campaigns were undertaken in several Antarctic areas comprising the Ross Sea. In this region, the 2008 NIWA IPY-CAML voyage obtained benthos samples from shelf to abyssal depths. In the present study, we focus on the Mollusca from this expedition and on the possible variations in their richness and composition with latitude and depth. Given the use of sampling gears selective for different size fractions of the macrofauna, we also assess which size fraction contained the highest biodiversity. Differences were detected in species composition with latitude (averaged across depth groups) but not for depth (averaged across latitudinal groups). Richness varied locally and showed a variety of patterns depending on the areas and depths considered. The greatest diversity of molluscs was found in the fine fraction (i.e., <4.1 mm) where a considerable number of species corresponded to new species or new regional records. Rarity was high with up to ~41% of species represented by single individuals and ~63% occurring at one station only. Fine-mesh trawling appears to be of fundamental importance in accelerating the census of the fine fraction, which is the one containing the highest diversity, and is recommended for future sampling in Antarctica and in polar areas in general.


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Authors: Ghiglione, Claudio, Alvaro, Maria Chiara, Piazza, Paola, Bowden, David, Griffiths, Huw J. ORCIDORCID record for Huw J. Griffiths, Carota, Cinzia, Nava, Consuelo Rubino, Schiaparelli, Stefano

On this site: Huw Griffiths
1 October, 2017
Polar Biology / 40
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