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Deep-sea suprabenthos assemblages (Crustacea) off the Balearic Islands (western Mediterranean): Mesoscale variability in diversity and production

TitoloDeep-sea suprabenthos assemblages (Crustacea) off the Balearic Islands (western Mediterranean): Mesoscale variability in diversity and production
Tipo di pubblicazioneArticolo su Rivista peer-reviewed
Anno di Pubblicazione2011
AutoriCartes, J.E., Mamouridis V., and Fanelli E.
RivistaJournal of Sea Research
Volume65
Paginazione340-354
ISSN13851101
Parole chiaveAmphipoda, Andaniexis mimonectes, Balearic Islands, benthic boundary layer, benthos, bioindicator, biological production, Biomass, Caprellida, carnivore, community composition, Crustacea, crustacean, Cumacea, Deep sea, detritus, environmental disturbance, Euphausiidae, Gammaridea, habitat structure, Hyperiidae, Isopoda, Lepechinella, Majorca, Mediterranean Sea, Mysida, omnivory, organic matter, Peracarida, Rhachotropis, Sampling, Seasonality, shelf break, Spain, water mass, zooplankton
Abstract

The composition of suprabenthic crustacean assemblages, their diversity, production (P) and production/biomass (P/B) ratios, were analyzed at species level along two transects situated to the north (N) and south (S) of Mallorca (Balearic Islands, western Mediterranean) at depths between 134. m and 760. m, based on a ca. bi-monthly sampling performed between August 2003 and June 2004. Differences with depth and season in assemblage composition and diversity were analyzed as a function of the contrasting environmental features (e.g. water mass dynamics) of the two areas. We identified 187 species (18 decapods, 5 euphausiids, 16 mysids, 76 gammaridean amphipods, 13 hyperiids, 1 caprellid, 21 isopods and 37 cumaceans). Substantial mesoscale variability in the deep-sea suprabenthic assemblages coupled with diversity trends between the N and S transects were found. Seasonality was the most important gradient influencing the dynamics of suprabenthos over the upper (350. m) and middle (650-750. m) slope in the N area. Conversely, the S area appeared to be more stable temporally with depth as the main gradient inducing assemblage differences. Different depth-related patterns were observed both for diversity and P/B. To the north diversity was very low at the shelf-break, increasing on the upper-slope (H'> 3.00) and then decreasing again on the middle-slope. To the south diversity increased smoothly downward, reaching the highest values on the middle-slope. Regarding productivity, P/B was highest at intermediate depths to the north (over ca. 450-500. m), while to the south highest P/Bs were found deeper (over ca. 600-650. m). The higher P/B at intermediate depths found along N are likely due to higher % of organic matter (OM) in sediments, a product of oceanographic frontal systems. In particular, P/B was higher along N among omnivores and detritus feeders (e.g. Andaniexis mimonectes, Lepechinella manco and combined cumaceans), coupled to enriched OM in sediments, while along S mesoplanktonic carnivores (Rhachotropis spp.) had higher P/Bs. We conclude that on the north slope the influence of frontal systems and more active flow dynamics of different water masses (WIW and LIW) increases natural disturbance in the area, increasing productivity and diversity of suprabenthic peracarids in the Benthic Boundary Layer. Also, species showed a displacement of their average distributions (their Centres of Gravity, CoG) to shallower depths along N, which is another indicator of more favorable habitat conditions for suprabenthos in the 400-500. m range at N. © 2011 Elsevier B.V.

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URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-79954426024&doi=10.1016%2fj.seares.2011.02.002&partnerID=40&md5=b915d53e848315f3fcd34bbe5fc35ca8
DOI10.1016/j.seares.2011.02.002
Citation KeyCartes2011340