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at the Porcupine Abyssal Plain, NE Atlantic.

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1 at the Porcupine Abyssal Plain, NE Atlantic.
Functional shifts in abyssal nematodes: a 15-year period study ( ) at the Porcupine Abyssal Plain, NE Atlantic. Vasiliki Kalogeropoulou 1,2,3*, N. Lampadariou ¹, A.J. Gooday 4, P. Martinez Arbizu 2,3, A. Vanruesel 5 1Hellenic Centre for Marine Research, P.O. Box 2214, Heraklion, Crete, 71003, Greece 2 University of Oldenburg, Department of Biology, Oldenburg, 26129, Germany 3DZM3 German Centre for Marine Biodiversity Research, Senckenberg am Meer, 26382,Wilhelmshaven, Germany 4Ocean Biogeochemistry and Ecosystems Research Group; National Oceanography Centre, Southampton SO14 3ZH, UK. 5Universiteit Gent; Faculteit Wetenschappen; Vakgroep Biologie; Afdeling Mariene Biologie Fig. 1. Charts showing (A) the general location of the Porcupine Abyssal Plain Sustained Observatory site PAP-SO, 48°50´N, 16°30´W) and (B) the disposition of samples assessed in the present study. Introduction Time series studies (>15 y) in abyssal benthic communities, conducted at the Porcupine Abyssal Plain in the NE Atlantic, at 4850 m water depth (Fig. 1), since 1989, have revealed long-term changes in megafaunal communities, possibly linked to climatic fluctuations that influence organic matter supply [1]. Observations at the PAP revealed a strong seasonal deposition of phytodetritus during some years and a radical shift in megafaunal abundance and community structure, notably a dramatic increase in densities of the holothurian Amperima rosea during ‘96-’04.This so-called ‘Amperima Event’ [2] is believed to be related to changes in the quantity and quality of organic matter reaching the seafloor [3]. A similar phenomenon, also possibly linked to climatic oscillations, was observed at the Station M in the NE Pacific (34°50´N, 123°00´W) [4]. Smaller size classes of the benthic community, the meiofauna [5], the foraminiferans [6] and the macrofauna [7], have also exhibited population changes over the course of the PAP time series. Nematodes, the dominant meiofaunal taxon at the PAP (’89-’04), exhibited a 3-fold increase in abundance since 1996 (Fig.2) apparently influenced by the upward trend in organic matter fluxes and the macro- and mega-faunal activity. Correlations with fluxes, however, were weak and flux peaks did not coincide with density peaks, indicating a time-lagged response [5]. The most abundant species exhibited temporal variations and shifts in assemblage composition That were due to the substitution of rare species between the “pre-Amperima” &“Amperima” periods. Unlike the temporal trend in densities, nematode species richness decreased during the Amperima period, shifting to a community defined mainly by opportunistic species. September ‘96 and March ‘97 was a transitional period for the nematodes, unlike the larger size categories, particularly the megafauna, which exhibited an immediate response[8]. In the present study the temporal variability in biomass and functional diversity were investigated taking into account the size spectra and functional complexity of the nematode assemblages. Combining biomass data and a range of biological traits based on buccal morphology, tail shape, body size, body shape and life history strategy, the questions below were addressed: 1. Are there any temporal variations in nematode size and biomass triggered by the changes observed in 1996? 2. Are there any temporal variations in nematode biological traits due to changes in environmental conditions? 3. Do the community shifts observed in nematode assemblages exhibit a stronger signal through a functional group approach? Fig. 2. Temporal variability in nematode densities (Ind.*10cm²), particulate organic carbon flux (g*m-2*yr-1) and biomass (μgr). Biological Traits Low values of the trophic index indicated a highly diverse community, when referring to feeding strategies. Selective deposit feeders increased with time due to the increased food supply. Non-selective deposit feeders and epigrowth feeders exhibited a significant 3-fold & 2-fold increase during the Amperima period. Large predators were only marginally present, due to the lack of freshly dead organisms. The three feeding groups coexist in large numbers since July ’97 indicating a variability in size, shape and quality of the available food and thus an efficient resource partitioning is accomplished amongst several nematode species with similar food preferences. Tail shape group proportions were significantly variable providing ecological information not incorporated in the rest of the biological trait groupings since particular tail shapes were not restricted to particular buccal morphologies. 50% of the species had elongated/filiform tails, being favoured during the Amperima period due to their locomotion capabilities. Small and slender nematodes dominated the assemblages (82%) presenting a significant 2-fold increase during the Amperima period. Although stout nematode densities were incomparable to the slender ones, their presence was functionally substantial to the assemblage in a long temporal scale. Long and large (>2mm) nematodes, which are known to inhabit usually the deeper sediment layers, were immediately influenced by the Amperima event as they increased significantly their low in general densities during the Transition period and decreased again from July ‘97 onwards, when small and slender nematodes took over. Colonisers (c-p2) were substantially more abundant (40%), yet groups with intermediate characteristics (c-p3) and persisters (c-p4) depicted high proportions to the total nematode assemblage as well (33% & 27%). The decreasing temporal trend in the Maturity index (MI) indicated an increasing microbial activity and a predominance of colonisers during the Amperima years. Assuming that prior to ‘96 the PAP was a stable habitat characterized by a range of species with narrow ecological niches, disturbance caused by the increased fluxes and the intense megabenthic activity influenced the most sensitive species the niches of which remained vacant or were filled gradually by less specialised species or species with a higher reproductive potential, resulting in a decreasing Maturity Index. Table 1. Temporal trends in nematode density, size spectra, buccal morphology, tail shape, life history strategy, body shape, body length and functional indices at the PAP ( ). ANOVA results are shown for between periods (’91-’94 vs. ’96-’97 Mar vs. ‘97July-’04), years and cruises (time points) comparisons. (ns - not significant). 180 nematode species were pooled into 56 functional groups. The biological traits matrix (Fig. 5a) revealed the predominance of 5 functional groups which belong to 3 functional complexes exhibiting significant contribution to the observed temporal variability. The most dominant functional complex, plus the first to respond to the Amperima event, consisted of c-p3 epigrowth feeding slender chromadorids (Acantholaimus, Chromadorita, etc.), bearing 2 different locomotion strategies. The second functional complex consisted of c-p2 deposit feeding slender monhysterids (Thalassomonhystera, Theristus, etc.) and the last important functional complex consisted of c-p4 selective deposit feeding corpulent Desmoscolecoidea (Desmoscolex, Tricoma, etc.). The 2nd stage MDS (Fig. 5b) revealed a significant separate clustering between the functional groups densities matrix (BTM) and the single functional characteristics matrices (rs=0.58) as well as the taxonomical densities and biomass matrices (rs=0.65). Fig. 5. a) nMDS ordination plot based on the presence/ absence Biological Traits Matrix and b) 2nd stage MDS ordination plot of inter-matrix rank correlations. Nematode biomass and size spectra Nematodes at the PAP were on average μm long, μm wide, with a L:W ratio of 28, being consistent with the general tendency for small sized nematodes at the deep sea areas worldwide. Total biomass was 40.2 μgr/10cm² and individual biomass 0.36 μgr . Temporally, nematode length and width deviated from the average (Fig.3) exhibiting a significant increase (L: μm;W: μm) during the Transition period (September ‘96 & March ‘97), a year after the first significant increase of downward fluxes coinciding, simultaneously, with the population explosion of holothurians. During the Amperima period, from July ‘97 onwards, both length and width (L: μm;W: μm) decreased significantly, resulting in an assemblage where slender and small sized nematodes predominated. Total biomass, on the other hand, exhibited an increasing trend ranging between μgr/10cm2 with two substantial peaks in September ‘96 and October ’02. A correlation between food availability and nematode size and biomass was revealed, yet with a time delay between maximum food supply and maximum growth of the nematodes, indicating a time lagged response of the nematode assemblages to the increased input of POC fluxes. Fig. 3. Temporal variation of nematode size spectra at the PAP ( ): average biomass displayed on X2 geometric weight classes (a); Average length (b) and length/width ratio on linear scale (c). The small nematode size in the deep sea is optimal, and deviations only occur when environmental conditions change. ABC curves (Fig. 4) revealed a moderately disturbed nematode assemblage in September ‘96 and March ’97 which coincided with the population explosion of the holothurians. This emphasized the significant biochemical changes of the benthic environment at the specific time points and supported the proposed Transition period that nematodes went through before responding to the increased phytodetritus fluxes and going back to an undisturbed condition from July ‘97 onwards. The substantial impact of the stability or not of the sediment biogeochemical conditions on the nematode size and taxonomic structure could be an explanation of their different response to the deep-sea environment compared to other benthic organisms. Fig.4. Abundance/Biomass comparison method (ABC) plots detecting the undisturbed, moderately disturbed or disturbed condition of the nematode assemblages at the PAP ( ). Conclusions The temporal changes observed in the size spectrum of the nematode assemblages at the PAP supported the corresponding food availability related shifts in their species composition. Significant biogeochemical changes took place in the benthic ecosystem at the PAP during ‘96 and March ’97 creating a moderately disturbed nematode assemblages and evoking community composition shifts. This was clearly a Transition period for the nematode communities. All biological traits exhibited significant temporal variability indicating substantial functional shifts in the nematode assemblages in a long temporal scale.The biological traits matrix revealed the predominance of 3 functional trait combinations (functional group complexes) which were primarily responsible for the temporal variability observed. The significant separate clustering of matrices based on functional, taxonomical and size spectra characteristics revealed that the information provided by a single functional characteristic is not a mere reflection of the information provided by another, increasing at the same time the importance of taxonomic, functional and morphometric information to an integrated community structure analysis. The significance of several numerically less abundant species is revealed when they are incorporated, based on their biological trait characteristics, in functional groups which is totally overlooked in species diversity studies. Following a functional approach gives us a more detailed insight of the structure of nematode assemblages and their ecological functions. Further knowledge of species physiology is needed for the efficient interpretation of the functional structure results in order to identify the missing links and comprehend their functional purpose and importance in the benthic ecosystem. Literature [1] Billett DSM, et al. (2010). Long-term change in the abyssal NE Atlantic: The ‘Amperima Event’ revisited. Deep Sea Research Part II: Topical Studies in Oceanography 57: [2] Bett, B.J., et al. (2001). Temporal variability in phytodetritus and megabenthic activity at the seabed in the deep Northeast Atlantic. Progress in Oceanography, 50, [3] Wigham, B.D., et al. (2003). Is long-term change in the abyssal NE Atlantic driven by qualitative changes in export flux? Progress in oceanography, 59, [4] Ruhl, H.A., (2007). Abundance and size distribution dynamics of abyssal epibenthic megafauna in the northeast Pacific. Ecology, 88, [5] Kalogeropoulou V., et al. (2010). Temporal changes (1989–1999) in deep-sea metazoan meiofaunal assemblages on the Porcupine Abyssal Plain, NE Atlantic. Deep Sea Research II, 57: [6] Gooday AJ, et al., (2010). Decadal-scale changes in shallow-infaunal foraminiferal assemblages at the Porcupine Abyssal Plain, NE Atlantic. Deep Sea Research II 57: [7] Soto EH, et al., (2010). Temporal variability in polychaete assemblages of the abyssal NE AtlanticOcean. Deep Sea Research II 57: [8] Kalogeropoulou V, et al., (unpublished). Temporal variability in community structure and diversity of deep sea meiobenthic nematodes and copepods in the Porcupine Abyssal Plain, NE Atlantic: a fifteen-year period study ( ) (Progress in Oceanography). MarBEF (Marine Biodiversity and Ecosystem Functioning) an EU funded network of excellence, consisting of 94 marine institutes, is a platform to integrate and disseminate knowledge and expertise on marine biodiversity, with links to researchers, industry, stakeholders and the general public. DEEPSETS: Deep-sea & Extreme Environments, Patterns of Species and Ecosystem Time Series is a responsive mode project undertaken within the MarBEF EU Network of Excellence, funded under the 6th Framework Programme of the European Union To find out more about HCMR, please visit:


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