Ontogenetic Changes in the Feeding Strategy of Lepidonotothen Nudifrons
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Global Diversity of Marine Isopods (Except Asellota and Crustacean Symbionts)
Collection Review Global Diversity of Marine Isopods (Except Asellota and Crustacean Symbionts) Gary C. B. Poore1*, Niel L. Bruce2,3 1 Museum Victoria, Melbourne, Victoria, Australia, 2 Museum of Tropical Queensland and School of Marine and Tropical Biology, James Cook University, Townsville, Queensland, Australia, 3 Department of Zoology, University of Johannesburg, Auckland Park, South Africa known from the supralittoral and intertidal to depths in excess of Abstract: The crustacean order Isopoda (excluding six kilometres. Isopods are a highly diverse group of crustaceans, Asellota, crustacean symbionts and freshwater taxa) with more than 10,300 species known to date, approximately comprise 3154 described marine species in 379 genera 6,250 of these being marine or estuarine. In the groups under in 37 families according to the WoRMS catalogue. The discussion here (about half the species) the vast majority of species history of taxonomic discovery over the last two centuries are known from depths of less than 1000 metres. is reviewed. Although a well defined order with the Peracarida, their relationship to other orders is not yet The Isopoda is one of the orders of peracarid crustaceans, that resolved but systematics of the major subordinal taxa is is, those that brood their young in a marsupium under the body. relatively well understood. Isopods range in size from less They are uniquely defined within Peracarida by the combination than 1 mm to Bathynomus giganteus at 365 mm long. of one pair of uropods attached to the pleotelson and pereopods of They inhabit all marine habitats down to 7280 m depth only one branch. Marine isopods are arguably the most but with few doubtful exceptions species have restricted morphologically diverse order of all the Crustacea. -
Crustacea, Malacostraca)*
SCI. MAR., 63 (Supl. 1): 261-274 SCIENTIA MARINA 1999 MAGELLAN-ANTARCTIC: ECOSYSTEMS THAT DRIFTED APART. W.E. ARNTZ and C. RÍOS (eds.) On the origin and evolution of Antarctic Peracarida (Crustacea, Malacostraca)* ANGELIKA BRANDT Zoological Institute and Zoological Museum, Martin-Luther-King-Platz 3, D-20146 Hamburg, Germany Dedicated to Jürgen Sieg, who silently died in 1996. He inspired this research with his important account of the zoogeography of the Antarctic Tanaidacea. SUMMARY: The early separation of Gondwana and the subsequent isolation of Antarctica caused a long evolutionary his- tory of its fauna. Both, long environmental stability over millions of years and habitat heterogeneity, due to an abundance of sessile suspension feeders on the continental shelf, favoured evolutionary processes of “preadapted“ taxa, like for exam- ple the Peracarida. This taxon performs brood protection and this might be one of the most important reasons why it is very successful (i.e. abundant and diverse) in most terrestrial and aquatic environments, with some species even occupying deserts. The extinction of many decapod crustaceans in the Cenozoic might have allowed the Peracarida to find and use free ecological niches. Therefore the palaeogeographic, palaeoclimatologic, and palaeo-hydrographic changes since the Palaeocene (at least since about 60 Ma ago) and the evolutionary success of some peracarid taxa (e.g. Amphipoda, Isopo- da) led to the evolution of many endemic species in the Antarctic. Based on a phylogenetic analysis of the Antarctic Tanaidacea, Sieg (1988) demonstrated that the tanaid fauna of the Antarctic is mainly represented by phylogenetically younger taxa, and data from other crustacean taxa led Sieg (1988) to conclude that the recent Antarctic crustacean fauna must be comparatively young. -
Notothenioid Lepidonotothen Nudifrons
J Comp Physiol B (1999) 169: 597±604 Ó Springer-Verlag 1999 ORIGINAL PAPER I. Hardewig á L. S. Peck á H. O. PoÈ rtner Thermal sensitivity of mitochondrial function in the Antarctic Notothenioid Lepidonotothen nudifrons Accepted: 2 September 1999 Abstract The thermal sensitivity of mitochondrial Introduction function was investigated in the stenothermal Antarctic ®sh Lepidonotothen nudifrons. State 3 respiration in- The Antarctic marine fauna is constantly exposed to creases with increasing temperature between 0 °C and extremely low temperatures only ranging between 18 °C with a Q of 2.43±2.63. State 4 respiration in the 10 )1.8 °C and 1 °C. Organisms inhabiting the extreme presence of oligomycin, an inhibitor of mitochondrial Antarctic environment must have developed special ATP synthase, quanti®es the leakage of protons through physiological adaptations to overcome the adverse the inner mitochondrial membrane, which causes oxygen eects of low temperatures on metabolism. consumption without concomitant ATP production. Despite uncompensated low resting metabolic rates This parameter shows an unusually high Q of 10 (Clarke 1991), polar animals show a compensatory in- 4.21 0.42 (0±18 °C), which indicates that proton crease in tissue oxidative capacity (van Dijk et al. 1998), leakage does not depend merely on ion diusion but is which is re¯ected in higher mitochondrial densities an enzyme-catalysed process. The dierential thermal compared to temperate zone animals (Archer and sensitivity of oxidative phosphorylation (=state 3) and Johnston 1991; Johnston et al. 1998). Accordingly, some proton leakage (=state 4 in the presence of oligomycin) oxidative enzymes show 1.5 to 5-fold increased maximal leads to progressive uncoupling of the mitochondria and activities in Antarctic ®sh tissues (Crockett and Sidell decreased eciency of oxidative phosphorylation under 1990). -
Microsatellite Markers for the Notothenioid Fish Lepidonotothen
Papetti et al. BMC Res Notes (2016) 9:238 DOI 10.1186/s13104-016-2039-x BMC Research Notes SHORT REPORT Open Access Microsatellite markers for the notothenioid fish Lepidonotothen nudifrons and two congeneric species Chiara Papetti1*, Lars Harms1, Jutta Jürgens1, Tina Sandersfeld1,2, Nils Koschnick1, Heidrun Sigrid Windisch1,3, Rainer Knust1, Hans‑Otto Pörtner1 and Magnus Lucassen1 Abstract Background: Loss of genetic variability due to environmental changes, limitation of gene flow between pools of individuals or putative selective pressure at specific markers, were previously documented for Antarctic notothenioid fish species. However, so far no studies were performed for the Gaudy notothen Lepidonotothen nudifrons. Starting from a species-specific spleen transcriptome library, we aimed at isolating polymorphic microsatellites (Type I; i.e. derived from coding sequences) suitable to quantify the genetic variability in this species, and additionally to assess the population genetic structure and demography in nototheniids. Results: We selected 43,269 transcripts resulting from a MiSeq sequencer run, out of which we developed 19 primer pairs for sequences containing microsatellite repeats. Sixteen loci were successfully amplified in L. nudifrons. Eleven microsatellites were polymorphic and allele numbers per locus ranged from 2 to 17. In addition, we amplified loci identified from L. nudifrons in two other congeneric species (L. squamifrons and L. larseni). Thirteen loci were highly transferable to the two congeneric species. Differences in polymorphism among species were detected. Conclusions: Starting from a transcriptome of a non-model organism, we were able to identify promising polymor‑ phic nuclear markers that are easily transferable to other closely related species. These markers can be a key instru‑ ment to monitor the genetic structure of the three Lepidonotothen species if genotyped in larger population samples. -
Marine Richness and Gradients at Deception Island, Antarctica DAVID K.A
Antarctic Science 20 (3), 271–279 (2008) & Antarctic Science Ltd 2008 Printed in the UK doi: 10.1017/S0954102008001090 Marine richness and gradients at Deception Island, Antarctica DAVID K.A. BARNES*, KATRIN LINSE, PETER ENDERLEIN, DAN SMALE, KEIRON P.P. FRASER and MATT BROWN British Antarctic Survey, NERC, High Cross, Madingley Road, Cambridge CB3 OET, UK *[email protected] Abstract: Studies of the recovery of the fauna following the 1967–70 eruptions at Deception Island, South Shetland Islands, have made it one of the best-studied marine sites of the Southern Ocean for biodiversity. Using SCUBA we surveyed the mega- and macro-epifauna of its subtidal zones in the entrance (Neptune’s Bellows), immediately inside the caldera (Whaler’s Bay) and well within the caldera (Fumarole Bay). Richness declined from 10 phyla, 13 classes and 35 species at Neptune’s Bellows to three phyla, four classes and five species in Whaler’s Bay and just two phyla, classes and species at Fumarole Bay. Amongst the 35 species we found at Neptune’s Bellows, 14 were previously unrecorded from Deception Island. Despite many ship visits and amongst the warmest sea temperatures in the Southern Ocean, the Non Indigenous Species (NIS) algae were not found in our survey. Deception Island has been recolonized considerably since the recent eruptions, but many taxa are still very poorly represented and the colonizers present are mainly those with planktotrophic larvae. Examination of the literature revealed that to date 163 named marine species have been found within the caldera as well as at least 50 more morphospecies, which are yet to be identified. -
Spawning Behaviour and Early Development in the Naked Dragonfish Gymnodraco Acuticeps CLIVE W
Antarctic Science 17 (3), 000–000 (2005) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102005 Spawning behaviour and early development in the naked dragonfish Gymnodraco acuticeps CLIVE W. EVANS1*, PAUL CZIKO2, CHI-HING CHRISTINA CHENG2 and ARTHUR L. DEVRIES2 1Molecular Genetics and Development, School of Biological Sciences, University of Auckland, Private Bag 92019, Auckland, New Zealand 2Department of Animal Biology, University of Illinois at Urbana-Champaign, 515 Morrill Hall, 505 South Goodwin Avenue, Urbana, IL 61801, USA. *[email protected] Abstract: Nesting sites of the naked dragonfish Gymnodraco acuticeps have been identified in 15–35 m water under fast ice adjacent to McMurdo Station, making it possible to examine embryonic development and early larval growth. Egg-laying (predominantly in October) is preceded by a distinctive whirling behavioural pattern driven by the male prodding the side of the female’s abdomen. The eggs (3.42 ± 0.19 mm in diameter) are laid on rocks as a single adherent layer (c. 2500 per patch). Development is unusually protracted, the first cleavage occurring after about 24 hr at about -1.9ºC. Hatching occurs about 10 months post-fertilization, beginning soon after the sun rises above the horizon. During this period one of the parents may act as a guard in an attempt to keep predators at bay. Upon hatching, the larvae (12.09 ± 0.36 mm long) swim towards the surface ice where they presumably seek refuge. Yolk absorption is complete in about 15 days. Larvae (grown in aquaria at a density of 0.7 larvae l-1) display an average daily growth rate of 0.42% over nine weeks. -
2008-2009 Field Season Report Chapter 9 Antarctic Marine Living Resources Program NOAA-TM-NMFS-SWFSC-445
2008-2009 Field Season Report Chapter 9 Antarctic Marine Living Resources Program NOAA-TM-NMFS-SWFSC-445 Demersal Finfi sh Survey of the South Orkney Islands Christopher Jones, Malte Damerau, Kim Deitrich, Ryan Driscoll, Karl-Hermann Kock, Kristen Kuhn, Jon Moore, Tina Morgan, Tom Near, Jillian Pennington, and Susanne Schöling Abstract A random, depth-stratifi ed bottom trawl survey of the South Orkney Islands (CCAMLR Subarea 48.2) fi nfi sh populations was completed as part of Leg II of the 2008/09 AMLR Survey. Data collection included abundance, spatial distribution, species and size composition, demographic structure and diet composition of fi nfi sh species within the 500 m isobath of the South Orkney Islands. Additional slope stations were sampled off the shelf of the South Orkney Islands and in the northern Antarctic Peninsula region (Subarea 48.1). During the 2008/09 AMLR Survey: • Seventy-fi ve stations were completed on the South Orkney Island shelf and slope area (63-764 m); • Th ree stations were completed on the northern Antarctic Peninsula slope (623-759 m); • A total of 7,693 kg (31,844 individuals) was processed from 65 fi nfi sh species; • Spatial distribution of standardized fi nfi sh densities demonstrated substantial contrast across the South Orkney Islands shelf area; • Th e highest densities of pooled fi nfi sh biomass occurred on the northwest shelf of the South Orkney Islands, at sta- tions north of Inaccessible and Coronation Islands, and the highest mean densities occurred within the 150-250 m depth stratum; • Th e greatest species diversity of fi nfi sh occurred at deeper stations on the southern shelf region; • Additional data collection of environmental and ecological features of the South Orkney Islands was conducted in order to further investigate Antarctic fi nfi sh in an ecosystem context. -
Introduction
Arch. Archives Vol. 11 Fasc. 2 197-206 2003 Pol. Fish. of Polish Fisheries ANTARCTIC FISHES: THE CHEMICAL COMPOSITION OF MUSCLE, LIVER AND FOOD OF TWO NOTOTHENIOIDS Ewa Kamler Department of Antarctic Biology of the Polish Academy of Sciences, and the Stanis³aw Sakowicz Inland Fisheries Institute in Olsztyn, Poland ABSTRACT. A combination of low fat (6.1 and 4.8% of dry matter), high protein (78.6 and 84.3% d.m.) and mineral content (6.3 and 6.2% d.m.), as well as high moisture (80.8 and 81.7% of fresh matter), which is typical of Antarctic benthic fish, was found in the muscle of Notothenia coriiceps and Lepidonotothen nudifrons, respectively. Fish food items (whole amphipods) were high in minerals (34.3% d.m.) and poor in protein (39.1% d.m.), while macroalgae presented an association of high moisture (89% of wet matter), high minerals (36.5% d.m.), low lipids (1.8% d.m.) and very low protein (17.5% d.m.). The poor nutritional value of these food items seems to be compensated for by high food intake. Sulfur levels in fish tissues were negatively related to fish size. Sulfur and nitrogen were inter-correlated strongly and positively, and most of the sulfate is probably derived in muscle and liver from sulfur-containing amino acids. Key words: NOTOTHENIA CORIICEPS, LEPIDONOTOTHEN NUDIFRONS, CHEMICAL COMPOSITION, MUSCLE, LIVER, FOOD CHAIN INTRODUCTION Antarctic fish species grow slowly, mature late and produce few large eggs that have a protracted incubation time. These factors all contribute to the generally high vulnerability of these species to over-fishing. -
Biogeographic Atlas of the Southern Ocean
Census of Antarctic Marine Life SCAR-Marine Biodiversity Information Network BIOGEOGRAPHIC ATLAS OF THE SOUTHERN OCEAN CHAPTER 7. BIOGEOGRAPHIC PATTERNS OF FISH. Duhamel G., Hulley P.-A, Causse R., Koubbi P., Vacchi M., Pruvost P., Vigetta S., Irisson J.-O., Mormède S., Belchier M., Dettai A., Detrich H.W., Gutt J., Jones C.D., Kock K.-H., Lopez Abellan L.J., Van de Putte A.P., 2014. In: De Broyer C., Koubbi P., Griffiths H.J., Raymond B., Udekem d’Acoz C. d’, et al. (eds.). Biogeographic Atlas of the Southern Ocean. Scientific Committee on Antarctic Research, Cambridge, pp. 328-362. EDITED BY: Claude DE BROYER & Philippe KOUBBI (chief editors) with Huw GRIFFITHS, Ben RAYMOND, Cédric d’UDEKEM d’ACOZ, Anton VAN DE PUTTE, Bruno DANIS, Bruno DAVID, Susie GRANT, Julian GUTT, Christoph HELD, Graham HOSIE, Falk HUETTMANN, Alexandra POST & Yan ROPERT-COUDERT SCIENTIFIC COMMITTEE ON ANTARCTIC RESEARCH THE BIOGEOGRAPHIC ATLAS OF THE SOUTHERN OCEAN The “Biogeographic Atlas of the Southern Ocean” is a legacy of the International Polar Year 2007-2009 (www.ipy.org) and of the Census of Marine Life 2000-2010 (www.coml.org), contributed by the Census of Antarctic Marine Life (www.caml.aq) and the SCAR Marine Biodiversity Information Network (www.scarmarbin.be; www.biodiversity.aq). The “Biogeographic Atlas” is a contribution to the SCAR programmes Ant-ECO (State of the Antarctic Ecosystem) and AnT-ERA (Antarctic Thresholds- Ecosys- tem Resilience and Adaptation) (www.scar.org/science-themes/ecosystems). Edited by: Claude De Broyer (Royal Belgian Institute -
Fig. 1. (A) E(S100) from BG and for the Entire Atlantic Ocean by Latitude Shows Considerable Variation in the Weddell Sea Region, but in General Lower Than the EWA
WILSON: Antarctic Biodiversity: Previous "Insights" Overlooked. A reply to A. Brandt, A. Gooday et al. Nature 447: 307 (2007) 9 Fig. 1. (A) E(S100) from BG and for the entire Atlantic Ocean by latitude shows considerable variation in the Weddell Sea region, but in general lower than the EWA. The horizontal bars are placed at the mean of the previous SO values (1), for those from BG (2) and for the EWA (3). Fig. 1. (B) E(S100) by depth, horizontal bars numbered as in A, shows a positive trend between diversity and depth, with the exception that the Weddell Sea may have depressed diversity at greatest depths, and EWA has high diversity at all depths. G.D.F. Wilson: Antarctic Biodiversity: Previous "Insights" Overlooked. A reply to A. Brandt, A. Gooday et al. Nature 447: 307 (2007) Text Note 9. Citations and methods for the evaluation of the data presented in Brandt et al. (2007) in comparison to previous data from the Weddell Sea and elsewhere in the Atlantic Ocean. The original report of the data on Isopoda from the Atlantic Ocean was: Hessler & Wilson (The origin and biogeography of malacostracan crustaceans in the deep sea. In Evolution, Time and Space: The Emergence of the Biosphere (eds. Sims, R. W., Price, J. H. & Whalley, P. E. S.) 227-254 (Academic Press, London and New York, 1983). This article calculated E(Sn) to 500 individuals. These data were subsequently used in the articles: Poore, G. C. B. & Wilson, G. D. F. Marine species richness. Nature 361, 597- 598 (1993). -
Case Study in Herve Cove, Antarctica
Communication The Effect of Glacier Recession on Benthic and Pelagic Communities: Case Study in Herve Cove, Antarctica Marta Potocka 1,*, Anna Kidawa 1, Anna Panasiuk 2, Luiza Bielecka 3, Justyna Wawrzynek- Borejko 3, Weronika Patuła 3, Kornelia A. Wójcik 1, Joanna Plenzler 1, Tomasz Janecki 4 and Robert J. Bialik 1 1 Department of Antarctic Biology, Institute of Biochemistry and Biophysics, Polish Academy of Sciences, Pawinskiego St. 5a, 02-106 Warsaw, Poland 2 Department of Marine Plankton Research, Institute of Oceanography, Faculty of Oceanography and Geography, University of Gdańsk, Av. Marszalka Pilsudskiego 46, 81-378 Gdynia, Poland 3 Department of Marine Ecosystems Functioning, Institute of Oceanography, Faculty of Oceanography and Geography, University of Gdańsk, Av. Marszalka Pilsudskiego 46, 81-378 Gdynia, Poland 4 Nencki Institute of Experimental Biology, Polish Academy of Sciences, Pasteura St. 3, 02-093 Warsaw, Poland * Correspondence: [email protected] Received: 29 June 2019; Accepted: 21 August 2019; Published: 24 August 2019 Abstract: Changes in macrobenthic and pelagic communities in the postglacial, partially isolated, lagoon Herve Cove in Admiralty Bay, King George Island, were investigated 15 years after the first comprehensive studies had been conducted in this region. The bottom area of the cove has enlarged from approximately 12 ha to 19 ha after the retreat of the Dera Icefall. Based on a photographic survey of the benthos and taxonomic composition of zooplankton, ecological succession and the colonization of new species have been observed. Several new species occur such as gastropods, seastars, sea urchins and isopods, and their presence in different parts of the cove, as well as breeding aggregations suggests that they reproduce there. -
Adaptation of Proteins to the Cold in Antarctic Fish: a Role for Methionine?
bioRxiv preprint doi: https://doi.org/10.1101/388900; this version posted August 9, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. Cold fish 1 Article: Discoveries 2 Adaptation of proteins to the cold in Antarctic fish: A role for Methionine? 3 4 Camille Berthelot1,2, Jane Clarke3, Thomas Desvignes4, H. William Detrich, III5, Paul Flicek2, Lloyd S. 5 Peck6, Michael Peters5, John H. Postlethwait4, Melody S. Clark6* 6 7 1Laboratoire Dynamique et Organisation des Génomes (Dyogen), Institut de Biologie de l'Ecole 8 Normale Supérieure ‐ UMR 8197, INSERM U1024, 46 rue d'Ulm, 75230 Paris Cedex 05, France. 9 2European Molecular Biology Laboratory, European Bioinformatics Institute, Wellcome Genome 10 Campus, Hinxton, Cambridge, CB10 1SD, UK. 11 3University of Cambridge, Department of Chemistry, Lensfield Rd, Cambridge CB2 1EW, UK. 12 4Institute of Neuroscience, University of Oregon, Eugene OR 97403, USA. 13 5Department of Marine and Environmental Sciences, Marine Science Center, Northeastern University, 14 Nahant, MA 01908, USA. 15 6British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, 16 Cambridge, CB3 0ET, UK. 17 18 *Corresponding Author: Melody S Clark, British Antarctic Survey, Natural Environment Research 19 Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK. Email: [email protected] 20 21 bioRxiv preprint doi: https://doi.org/10.1101/388900; this version posted August 9, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.