Lithodes Santolla (J.H
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Marine Ecology Progress Series 600:21
Vol. 600: 21–39, 2018 MARINE ECOLOGY PROGRESS SERIES Published July 30 https://doi.org/10.3354/meps12663 Mar Ecol Prog Ser OPENPEN ACCESSCCESS Short-term processing of ice algal- and phytoplankton- derived carbon by Arctic benthic communities revealed through isotope labelling experiments Anni Mäkelä1,*, Ursula Witte1, Philippe Archambault2 1School of Biological Sciences, University of Aberdeen, Aberdeen AB24 3UU, UK 2Département de biologie, Québec Océan, Université Laval, Québec, QC G1V 0A6, Canada ABSTRACT: Benthic ecosystems play a significant role in the carbon (C) cycle through remineral- ization of organic matter reaching the seafloor. Ice algae and phytoplankton are major C sources for Arctic benthic consumers, but climate change-mediated loss of summer sea ice is predicted to change Arctic marine primary production by increasing phytoplankton and reducing ice algal contributions. To investigate the impact of changing algal C sources on benthic C processing, 2 isotope tracing experiments on 13C-labelled ice algae and phytoplankton were conducted in the North Water Polynya (NOW; 709 m depth) and Lancaster Sound (LS; 794 m) in the Canadian Arc- tic, during which the fate of ice algal (CIA) and phytoplankton (CPP) C added to sediment cores was traced over 4 d. No difference in sediment community oxygen consumption (SCOC, indicative of total C turnover) between the background measurements and ice algal or phytoplankton cores was found at either site. Most of the processed algal C was respired, with significantly more CPP than CIA being released as dissolved inorganic C at both sites. Macroinfaunal uptake of algal C was minor, but bacterial assimilation accounted for 33−44% of total algal C processing, with no differences in bacterial uptake of CPP and CIA found at either site. -
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https://theses.gla.ac.uk/ Theses Digitisation: https://www.gla.ac.uk/myglasgow/research/enlighten/theses/digitisation/ This is a digitised version of the original print thesis. Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten: Theses https://theses.gla.ac.uk/ [email protected] ASPECTS OF THE BIOLOGY OF THE SQUAT LOBSTER, MUNIDA RUGOSA (FABRICIUS, 1775). Khadija Abdulla Yousuf Zainal, BSc. (Cairo). A thesis submitted for the degree of Doctor of Philosophy to the Faculty of Science at the University of Glasgow. August 1990 Department of Zoology, University of Glasgow, Glasgow, G12 8QQ. University Marine Biological Station, Millport, Isle of Cumbrae, Scotland KA28 OEG. ProQuest Number: 11007559 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11007559 Published by ProQuest LLC(2018). -
A Year in Hypoxia: Epibenthic Community Responses to Severe Oxygen Deficit at a Subsea Observatory in a Coastal Inlet
A Year in Hypoxia: Epibenthic Community Responses to Severe Oxygen Deficit at a Subsea Observatory in a Coastal Inlet Marjolaine Matabos1,2*, Verena Tunnicliffe1,3, S. Kim Juniper1,2, Courtney Dean1 1 School of Earth and Ocean Sciences, University of Victoria, Victoria, BC, Canada, 2 NEPTUNE Canada, University of Victoria, Victoria, BC, Canada, 3 VENUS, University of Victoria, Victoria, BC, Canada Abstract Changes in ocean ventilation driven by climate change result in loss of oxygen in the open ocean that, in turn, affects coastal areas in upwelling zones such as the northeast Pacific. Saanich Inlet, on the west coast of Canada, is a natural seasonally hypoxic fjord where certain continental shelf species occur in extreme hypoxia. One study site on the VENUS cabled subsea network is located in the hypoxic zone at 104 m depth. Photographs of the same 5 m2 area were taken with a remotely-controlled still camera every 2/3 days between October 6th 2009 and October 18th 2010 and examined for community composition, species behaviour and microbial mat features. Instruments located on a near-by platform provided high-resolution measurements of environmental variables. We applied multivariate ordination methods and a principal coordinate analysis of neighbour matrices to determine temporal structures in our dataset. Responses to seasonal hypoxia (0.1–1.27 ml/l) and its high variability on short time-scale (hours) varied among species, and their life stages. During extreme hypoxia, microbial mats developed then disappeared as a hippolytid shrimp, Spirontocaris sica, appeared in high densities (200 m22) despite oxygen below 0.2 ml/l. -
Phytoplankton As Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate
sustainability Review Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate Samarpita Basu * ID and Katherine R. M. Mackey Earth System Science, University of California Irvine, Irvine, CA 92697, USA; [email protected] * Correspondence: [email protected] Received: 7 January 2018; Accepted: 12 March 2018; Published: 19 March 2018 Abstract: The world’s oceans are a major sink for atmospheric carbon dioxide (CO2). The biological carbon pump plays a vital role in the net transfer of CO2 from the atmosphere to the oceans and then to the sediments, subsequently maintaining atmospheric CO2 at significantly lower levels than would be the case if it did not exist. The efficiency of the biological pump is a function of phytoplankton physiology and community structure, which are in turn governed by the physical and chemical conditions of the ocean. However, only a few studies have focused on the importance of phytoplankton community structure to the biological pump. Because global change is expected to influence carbon and nutrient availability, temperature and light (via stratification), an improved understanding of how phytoplankton community size structure will respond in the future is required to gain insight into the biological pump and the ability of the ocean to act as a long-term sink for atmospheric CO2. This review article aims to explore the potential impacts of predicted changes in global temperature and the carbonate system on phytoplankton cell size, species and elemental composition, so as to shed light on the ability of the biological pump to sequester carbon in the future ocean. -
Podding of Paralomis Granulosa
Nauplius ORIGINAL ARTICLE Podding of Paralomis granulosa (Lithodidae) juveniles inhabiting kelp forests of the Cape Horn e-ISSN 2358-2936 www.scielo.br/nau Archipelago (Chile) www.crustacea.org.br Ivan Cañete1 orcid.org/0000-0002-1293-886X Alan M. Friedlander2,3 orcid.org/0000-0003-4858-006X Enric Sala2 orcid.org/0000-0003-4730-3570 Tania Figueroa1 orcid.org/0000-0003-4928-4924 1 Department of Sciences and Natural Resources, Faculty of Sciences, University of Magallanes. Punta Arenas, Chile. IC E-mail: [email protected] TF E-mail: [email protected] 2 Pristine Seas, National Geographic Society. Washington DC, United States of America ES E-mail: [email protected] 3 Hawaii Institute of Marine Biology, University of Hawaii. Kaneohe, Hawaii. United States of America. AMF E-mail: [email protected] ZOOBANK: http://zoobank.org/urn:lsid:zoobank.org:pub:A40E315A-4C8E-4FB7- A6CB-8AF9973CFBDF ABSTRACT Subtidal observations along the Cape Horn Archipelago, Chile (CHA) in February 2017 revealed an unusually large aggregation (or pod) of juvenile false king crabs, Paralomis granulosa (Hombron and Jacquinot, 1846), in association with kelp forests (Macrocystis pyrifera and Lessonia spp.). This is the first study to report a dense aggregation of juveniles of this crab, which was observed at Wollaston Island (WI) (~ 10 m). Paralomis granulosa was present on half the transects at WI (N=10), with a density of 3.1 ± 9.9 ind. m-2. Photographs from the podding event showed densities of P. granulosa ranging from 63 to 367 ind. plant-1 (190 ± 133 ind. plant-1). -
Challenging the Cold: Crabs Reconquer the Antarctic
Ecology, 86(3), 2005, pp. 619±625 q 2005 by the Ecological Society of America CHALLENGING THE COLD: CRABS RECONQUER THE ANTARCTIC SVEN THATJE,1,5 KLAUS ANGER,2 JAVIER A. CALCAGNO,3 GUSTAVO A. LOVRICH,4 HANS-OTTO POÈ RTNER,1 AND WOLF E. ARNTZ1 1Alfred Wegener Institute for Polar and Marine Research, Columbusstr. D-27568 Bremerhaven, Germany 2Biologische Anstalt Helgoland, Foundation Alfred Wegener Institute, Helgoland, Germany 3Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Intendente GuÈiraldes 2160, C1428EHA, Buenos Aires, Argentina 4Consejo Nacional de Investigaciones Cientõ®cas y TeÂcnicas, Centro Austral de Investigaciones Cientõ®cas, CC 92, V9410BFD Ushuaia, Tierra del Fuego, Argentina Abstract. Recent records of lithodid crabs in deeper waters off the Antarctic continental slope raised the question of the return of crabs to Antarctic waters, following their extinction in the lower Miocene ;15 million years ago. Antarctic cooling may be responsible for the impoverishment of the marine high Antarctic decapod fauna, presently comprising only ®ve benthic shrimp species. Effects of polar conditions on marine life, including lowered metabolic rates and short seasonal food availability, are discussed as main evolutionary driving forces shaping Antarctic diversity. In particular, planktotrophic larval stages should be vulnerable to the mismatch of prolonged development and short periods of food avail- ability, selecting against complex life cycles. We hypothesize that larval lecithotrophy and cold tolerance, as recently observed in Subantarctic lithodids, represent, together with other adaptations in the adults, key features among the life-history adaptations of lithodids, potentially enabling them to conquer polar ecosystems. The return of benthic top predators to high Antarctic waters under conditions of climate change would considerably alter the benthic communities. -
Changes in Biomass and Chemical Composition During Lecithotrophic Larval Development of the Southern Stone Crab Paralomis Granulosa
MARINE ECOLOGY PROGRESS SERIES Vol. 257: 189–196, 2003 Published August 7 Mar Ecol Prog Ser Changes in biomass and chemical composition during lecithotrophic larval development of the southern stone crab Paralomis granulosa Javier A. Calcagno1,*, Sven Thatje2, Klaus Anger3, Gustavo A. Lovrich4, Antje Kaffenberger3 1Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Intendente Güiraldes 2160, Lab 64, 4to Piso, Pab II, Cdad Universitaria C1428EHA, Buenos Aires, Argentina 2Alfred Wegener Institute for Polar and Marine Research, PO Box 120 161, 27515 Bremerhaven, Germany 3Biologische Anstalt Helgoland, Stiftung Alfred Wegener Institute for Polar and Marine Research, 27498 Helgoland, Germany 4Consejo Nacional de Investigaciones Científicas y Técnicas, Centro Austral de Investigaciones Científicas, CADIC, CC 92, V9410BFD Ushuaia, Tierra del Fuego, Argentina ABSTRACT: Changes in biomass and elemental composition (dry mass, W; carbon, C; nitrogen, N; hy- drogen, H) were studied in the laboratory during complete larval and early juvenile development of the southern stone crab Paralomis granulosa (Jacquinot). At 6 ± 0.5°C; total larval development from hatching to metamorphosis lasted ca. 56 d, comprising 2 demersal zoeal stages and a benthic mega- lopa, with mean stage durations of 5, 11 and 45 d, respectively. All larval stages of P. granulosa are lecithotrophic, and first feeding and growth were consistently observed immediately after meta- morphosis to the first juvenile crab stage. Regardless of presence or absence of food, W, C, N, and H decreased throughout larval development. Also the C:N mass ratio decreased significantly, from 7.2 at hatching to 4.2 at metamorphosis, indicating that a large initial lipid store remaining from the egg yolk was gradually utilised as an internal energy source. -
Proceedings of the United States National Museum
descriptions of a new genus and forty-six new spp:cies of crusta(jeans of the family GALA- theid.e, with a list of the known marine SPECIES. By James E. Benedict, Assistant Curator of Marine Invertebrates. The collection of Galatheids in the United States National Museum, upon which this paper is based, began with the first dredgings of the U. S. Fish Commission steamer Albatross in 1883, and has grown as that busy ship has had opportunit}' to dredge. During the first period of its work many of the species taken were identical with those found by the U. S. Coast Survey steamer JBlake, afterwards described by A. Milne-Edwards, and in addition several new species were collected. During the voyage of the Albatross to the Pacific Ocean through the Straits of Magellan interesting addi- tions were made to the collection. Since then the greater part of the time spent by the Albatross at sea has been in Alaskan waters, where Galatheids do not seem to abound. However, occasional cruises else- where have greatly enriched the collection, notably three—one in the Gulf of California, one to the Galapagos Islands, and one to the coast of Japan and southward. The U. S. National Museum has received a number of specimens from the Museum of Natural History, Paris, and also from the Indian Museum, Calcutta. The literature of the deep-sea Galatheidie from the nature of the case is not greatly scattered. The first considerate number of species were described by A. Milne-Edwards from dredgings made by the Blake in the West Indian region. -
Intern Report
Insights from abyssal lebensspuren Jennifer Durden, University of Southampton, UK Mentors: Ken Smith, Jr., Christine Huffard, Katherine Dunlop Summer 2014 Keywords: lebensspuren, traces, abyss, megafauna, deposit-feeding, benthos, sediment ABSTRACT The seasonal input of food to the abyss impacts the benthic community, and changes to that temporal cycle, through changes to the climate and surface ocean conditions impact the benthic assemblage. Most of the benthic fauna are deposit feeders, and many leave traces (‘lebensspuren’) of their activity in the sediment. These traces provide an avenue for examining the temporal variations in the activity of these animals, with insights into the usage of food inputs to the system. Traces of a variety of functions were identified in photographs captured in 2011 and 2012 from Station M, a soft-sedimented abyssal site in the northeast Pacific. Lebensspuren creation, holothurian tracking, and lebensspuren duration were estimated from hourly time-lapse images, while trace densities, diversity and seabed coverage were assessed from photographs captured with a seabed- transiting vehicle. The creation rates and duration of traces on the seabed appeared to vary over time, and may have been related to food supply, as may tracking rates of holothurians. The density, diversity and seabed coverage by lebensspuren of different types varied with food supply, with different lag times for POC flux and salp coverage. These are interpreted to be due to selectivity of 1 deposit feeders, and different response times between trace creators. These variations shed light on the usage of food inputs to the abyss. INTRODUCTION Deep-sea benthic communities rely on a seasonal food supply of detritus from the surface ocean (Billett et al., 1983, Rice et al., 1986). -
Drivers and Effects of Karenia Mikimotoi Blooms in the Western English Channel ⇑ Morvan K
Progress in Oceanography 137 (2015) 456–469 Contents lists available at ScienceDirect Progress in Oceanography journal homepage: www.elsevier.com/locate/pocean Drivers and effects of Karenia mikimotoi blooms in the western English Channel ⇑ Morvan K. Barnes a,1, Gavin H. Tilstone a, , Timothy J. Smyth a, Claire E. Widdicombe a, Johanna Gloël a,b, Carol Robinson b, Jan Kaiser b, David J. Suggett c a Plymouth Marine Laboratory, Prospect Place, West Hoe, Plymouth PL1 3DH, UK b Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK c Functional Plant Biology & Climate Change Cluster, University of Technology Sydney, PO Box 123, Broadway, NSW 2007, Australia article info abstract Article history: Naturally occurring red tides and harmful algal blooms (HABs) are of increasing importance in the coastal Available online 9 May 2015 environment and can have dramatic effects on coastal benthic and epipelagic communities worldwide. Such blooms are often unpredictable, irregular or of short duration, and thus determining the underlying driving factors is problematic. The dinoflagellate Karenia mikimotoi is an HAB, commonly found in the western English Channel and thought to be responsible for occasional mass finfish and benthic mortali- ties. We analysed a 19-year coastal time series of phytoplankton biomass to examine the seasonality and interannual variability of K. mikimotoi in the western English Channel and determine both the primary environmental drivers of these blooms as well as the effects on phytoplankton productivity and oxygen conditions. We observed high variability in timing and magnitude of K. mikimotoi blooms, with abun- dances reaching >1000 cells mLÀ1 at 10 m depth, inducing up to a 12-fold increase in the phytoplankton carbon content of the water column. -
California “Epicaridean” Isopods Superfamilies Bopyroidea and Cryptoniscoidea (Crustacea, Isopoda, Cymothoida)
California “Epicaridean” Isopods Superfamilies Bopyroidea and Cryptoniscoidea (Crustacea, Isopoda, Cymothoida) by Timothy D. Stebbins Presented to SCAMIT 13 February 2012 City of San Diego Marine Biology Laboratory Environmental Monitoring & Technical Services Division • Public Utilities Department (Revised 1/18/12) California Epicarideans Suborder Cymothoida Subfamily Phyllodurinae Superfamily Bopyroidea Phyllodurus abdominalis Stimpson, 1857 Subfamily Athelginae Family Bopyridae * Anathelges hyphalus (Markham, 1974) Subfamily Pseudioninae Subfamily Hemiarthrinae Aporobopyrus muguensis Shiino, 1964 Hemiarthrus abdominalis (Krøyer, 1840) Aporobopyrus oviformis Shiino, 1934 Unidentified species † Asymmetrione ambodistorta Markham, 1985 Family Dajidae Discomorphus magnifoliatus Markham, 2008 Holophryxus alaskensis Richardson, 1905 Goleathopseudione bilobatus Román-Contreras, 2008 Family Entoniscidae Munidion pleuroncodis Markham, 1975 Portunion conformis Muscatine, 1956 Orthione griffenis Markham, 2004 Superfamily Cryptoniscoidea Pseudione galacanthae Hansen, 1897 Family Cabiropidae Pseudione giardi Calman, 1898 Cabirops montereyensis Sassaman, 1985 Subfamily Bopyrinae Family Cryptoniscidae Bathygyge grandis Hansen, 1897 Faba setosa Nierstrasz & Brender à Brandis, 1930 Bopyrella calmani (Richardson, 1905) Family Hemioniscidae Probopyria sp. A Stebbins, 2011 Hemioniscus balani Buchholz, 1866 Schizobopyrina striata (Nierstrasz & Brender à Brandis, 1929) Subfamily Argeiinae † Unidentified species of Hemiarthrinae infesting Argeia pugettensis -
Annotated Checklist of New Zealand Decapoda (Arthropoda: Crustacea)
Tuhinga 22: 171–272 Copyright © Museum of New Zealand Te Papa Tongarewa (2011) Annotated checklist of New Zealand Decapoda (Arthropoda: Crustacea) John C. Yaldwyn† and W. Richard Webber* † Research Associate, Museum of New Zealand Te Papa Tongarewa. Deceased October 2005 * Museum of New Zealand Te Papa Tongarewa, PO Box 467, Wellington, New Zealand ([email protected]) (Manuscript completed for publication by second author) ABSTRACT: A checklist of the Recent Decapoda (shrimps, prawns, lobsters, crayfish and crabs) of the New Zealand region is given. It includes 488 named species in 90 families, with 153 (31%) of the species considered endemic. References to New Zealand records and other significant references are given for all species previously recorded from New Zealand. The location of New Zealand material is given for a number of species first recorded in the New Zealand Inventory of Biodiversity but with no further data. Information on geographical distribution, habitat range and, in some cases, depth range and colour are given for each species. KEYWORDS: Decapoda, New Zealand, checklist, annotated checklist, shrimp, prawn, lobster, crab. Contents Introduction Methods Checklist of New Zealand Decapoda Suborder DENDROBRANCHIATA Bate, 1888 ..................................... 178 Superfamily PENAEOIDEA Rafinesque, 1815.............................. 178 Family ARISTEIDAE Wood-Mason & Alcock, 1891..................... 178 Family BENTHESICYMIDAE Wood-Mason & Alcock, 1891 .......... 180 Family PENAEIDAE Rafinesque, 1815 ..................................