Diel, Seasonal and Interannual Patterns in Zooplankton and Micronekton Species Composition in the Subtropical Atlantic
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Diversity and Community Structure of Pelagic Cnidarians in the Celebes and Sulu Seas, Southeast Asian Tropical Marginal Seas
Deep-Sea Research I 100 (2015) 54–63 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Diversity and community structure of pelagic cnidarians in the Celebes and Sulu Seas, southeast Asian tropical marginal seas Mary M. Grossmann a,n, Jun Nishikawa b, Dhugal J. Lindsay c a Okinawa Institute of Science and Technology Graduate University (OIST), Tancha 1919-1, Onna-son, Okinawa 904-0495, Japan b Tokai University, 3-20-1, Orido, Shimizu, Shizuoka 424-8610, Japan c Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 237-0061, Japan article info abstract Article history: The Sulu Sea is a semi-isolated, marginal basin surrounded by high sills that greatly reduce water inflow Received 13 September 2014 at mesopelagic depths. For this reason, the entire water column below 400 m is stable and homogeneous Received in revised form with respect to salinity (ca. 34.00) and temperature (ca. 10 1C). The neighbouring Celebes Sea is more 19 January 2015 open, and highly influenced by Pacific waters at comparable depths. The abundance, diversity, and Accepted 1 February 2015 community structure of pelagic cnidarians was investigated in both seas in February 2000. Cnidarian Available online 19 February 2015 abundance was similar in both sampling locations, but species diversity was lower in the Sulu Sea, Keywords: especially at mesopelagic depths. At the surface, the cnidarian community was similar in both Tropical marginal seas, but, at depth, community structure was dependent first on sampling location Marginal sea and then on depth within each Sea. Cnidarians showed different patterns of dominance at the two Sill sampling locations, with Sulu Sea communities often dominated by species that are rare elsewhere in Pelagic cnidarians fi Community structure the Indo-Paci c. -
Invert3 2 115 135 Abiahy at All.PM6
Invertebrate Zoology, 2006, 3(2): 115-135 INVERTEBRATE ZOOLOGY, 2006 published online 06.01.2007 accepted for publication 21.11.2006 Redescription of Limnoithona tetraspina Zhang et Li, 1976 (Copepoda, Cyclopoida) with a discussion of character states shared with the Oithonidae and older cyclopoids Bernardo Barroso do Abiahy\ Carlos Eduardo Falavigna da Rocha^, Frank D. Ferrari^ ' Avenida Manuel Hipolito do Rego 1270/ap. 09, 11.600-000 Sao Sebastiao, SP, Brasd ^ Universidade de Sao Paulo, Instituto de Biociencias, Departamento de Zoologia, Rua do Matdo, travessa 14, No. 321, 05508-900 Sao Paulo, Brazd 'Department of Invertebrate Zoology, MRC-534, National Museum of Natural History, Smithso- nian Institution, 4210 Silver Hill Rd., Suitland, MD 20746 U.S.A. ABSTRACT: Limnoithona tetraspina Zhang et Li, 1976 is redescribed, and the morpho- logy of the cephalosome, rostral area, oral appendages, legs 1-6 andurosome of adult males and females is illustrated. Morphological features separating L. tetraspina from its only congener,Z.5/«e«5;5, include: a more pronounced rostrum; 1 seta more on the proximal lobe of the basis of the maxillule; 1 seta more on the endopod of the maxillule; middle endopodal segment of swimming legs 2-A with 1 seta more; proximal and distal seta of the middle endopodal segment of swimming leg 4 with a flange; exopod of leg 5 with a proximal lateral seta; male cephalosome ventrally with pores with cilia. A rounded projection between labrum and rostrum is a shared derived state for both species of Limnoithona. Derived morphological features of the remaining species of Oithonidae, which are not shared with L. -
Ocean Deoxygenation and Copepods: Coping with Oxygen Minimum Zone Variability
Biogeosciences, 17, 2315–2339, 2020 https://doi.org/10.5194/bg-17-2315-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Ocean deoxygenation and copepods: coping with oxygen minimum zone variability Karen F. Wishner1, Brad Seibel2, and Dawn Outram1 1Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA 2College of Marine Science, University of South Florida, St. Petersburg, FL 33701, USA Correspondence: Karen F. Wishner ([email protected]) Received: 27 September 2019 – Discussion started: 28 October 2019 Revised: 31 March 2020 – Accepted: 2 April 2020 – Published: 24 April 2020 Abstract. Increasing deoxygenation (loss of oxygen) of compression concept). These distribution depths changed by the ocean, including expansion of oxygen minimum zones tens to hundreds of meters depending on the species, oxygen (OMZs), is a potentially important consequence of global profile, and phenomenon. For example, at the lower oxycline, warming. We examined present-day variability of vertical the depth of maximum abundance for Lucicutia hulsemannae distributions of 23 calanoid copepod species in the East- shifted from ∼ 600 to ∼ 800 m, and the depth of diapause for ern Tropical North Pacific (ETNP) living in locations with Eucalanus inermis shifted from ∼ 500 to ∼ 775 m, in an ex- different water column oxygen profiles and OMZ inten- panded OMZ compared to a thinner OMZ, but remained at sity (lowest oxygen concentration and its vertical extent in similar low oxygen levels in -
Tesis Estructura Comunitaria De Copepodos .Pdf
Universidad de Concepción Dirección de Postgrado Facultad de Ciencias Naturales y Oceanográficas Programa de Magister en Ciencias mención Oceanografía Estructura comunitaria de copépodos pelágicos asociados a montes submarinos de la Dorsal Juan Fernández (32-34°S) en el Pacífico Sur Oriental Tesis para optar al grado de Magíster en Ciencias con mención en Oceanografía PAMELA ANDREA FIERRO GONZÁLEZ CONCEPCIÓN-CHILE 2019 Profesora Guía: Pamela Hidalgo Díaz Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas Universidad de Concepción Profesor Co-guía: Rubén Escribano Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas Universidad de Concepción La Tesis de “Magister en Ciencias con mención en Oceanografía” titulada “Estructura comunitaria de copépodos pelágicos asociados a montes submarinos de la Dorsal Juan Fernández (32-34°S) en el Pacífico sur oriental”, de la Srta. “PAMELA ANDREA FIERRO GONZÁLEZ” y realizada bajo la Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, ha sido aprobada por la siguiente Comisión de Evaluación: Dra. Pamela Hidalgo Díaz Profesora Guía Universidad de Concepción Dr. Rubén Escribano Profesor Co-Guía Universidad de Concepción Dr. Samuel Hormazábal Miembro de la Comisión Evaluadora Pontificia Universidad Católica de Valparaíso Dr. Fabián Tapia Director Programa de Magister en Oceanografía Universidad de Concepción ii A Juan Carlos y Sebastián iii AGRADECIMIENTOS Agradezco a quienes con su colaboración y apoyo hicieron posible el desarrollo y término de esta tesis. En primer lugar, agradezco a los miembros de mi comisión de tesis. A mi profesora guía, Dra. Pamela Hidalgo, por apoyarme y guiarme en este largo camino de formación académica, por su gran calidad humana, contención y apoyo personal. -
Changing Jellyfish Populations: Trends in Large Marine Ecosystems
CHANGING JELLYFISH POPULATIONS: TRENDS IN LARGE MARINE ECOSYSTEMS by Lucas Brotz B.Sc., The University of British Columbia, 2000 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in The Faculty of Graduate Studies (Oceanography) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) October 2011 © Lucas Brotz, 2011 Abstract Although there are various indications and claims that jellyfish have been increasing at a global scale in recent decades, a rigorous demonstration to this effect has never been presented. As this is mainly due to scarcity of quantitative time series of jellyfish abundance from scientific surveys, an attempt is presented here to complement such data with non- conventional information from other sources. This was accomplished using the analytical framework of fuzzy logic, which allows the combination of information with variable degrees of cardinality, reliability, and temporal and spatial coverage. Data were aggregated and analysed at the scale of Large Marine Ecosystem (LME). Of the 66 LMEs defined thus far, which cover the world’s coastal waters and seas, trends of jellyfish abundance (increasing, decreasing, or stable/variable) were identified (occurring after 1950) for 45, with variable degrees of confidence. Of these 45 LMEs, the overwhelming majority (31 or 69%) showed increasing trends. Recent evidence also suggests that the observed increases in jellyfish populations may be due to the effects of human activities, such as overfishing, global warming, pollution, and coastal development. Changing jellyfish populations were tested for links with anthropogenic impacts at the LME scale, using a variety of indicators and a generalized additive model. Significant correlations were found with several indicators of ecosystem health, as well as marine aquaculture production, suggesting that the observed increases in jellyfish populations are indeed due to human activities and the continued degradation of the marine environment. -
High Abundance of Salps in the Coastal Gulf of Alaska During 2011
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/301733881 High abundance of salps in the coastal Gulf of Alaska during 2011: A first record of bloom occurrence for the northern Gulf Article in Deep Sea Research Part II Topical Studies in Oceanography · April 2016 DOI: 10.1016/j.dsr2.2016.04.009 CITATION READS 1 33 4 authors, including: Ayla J. Doubleday Moira Galbraith University of Alaska System Institute of Ocean Sciences, Sidney, BC, Cana… 3 PUBLICATIONS 16 CITATIONS 28 PUBLICATIONS 670 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: l. salmonis and c. clemensi attachment sites: chum salmon View project All content following this page was uploaded by Moira Galbraith on 10 June 2016. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Deep-Sea Research II ∎ (∎∎∎∎) ∎∎∎–∎∎∎ Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr2 High abundance of salps in the coastal Gulf of Alaska during 2011: A first record of bloom occurrence for the northern Gulf Kaizhi Li a, Ayla J. Doubleday b, Moira D. Galbraith c, Russell R. Hopcroft b,n a Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China b Institute of Marine Science, University of Alaska, Fairbanks, AK 99775-7220, USA c Institute of Ocean Sciences, Fisheries and Oceans Canada, P.O. -
Molecular Species Delimitation and Biogeography of Canadian Marine Planktonic Crustaceans
Molecular Species Delimitation and Biogeography of Canadian Marine Planktonic Crustaceans by Robert George Young A Thesis presented to The University of Guelph In partial fulfilment of requirements for the degree of Doctor of Philosophy in Integrative Biology Guelph, Ontario, Canada © Robert George Young, March, 2016 ABSTRACT MOLECULAR SPECIES DELIMITATION AND BIOGEOGRAPHY OF CANADIAN MARINE PLANKTONIC CRUSTACEANS Robert George Young Advisors: University of Guelph, 2016 Dr. Sarah Adamowicz Dr. Cathryn Abbott Zooplankton are a major component of the marine environment in both diversity and biomass and are a crucial source of nutrients for organisms at higher trophic levels. Unfortunately, marine zooplankton biodiversity is not well known because of difficult morphological identifications and lack of taxonomic experts for many groups. In addition, the large taxonomic diversity present in plankton and low sampling coverage pose challenges in obtaining a better understanding of true zooplankton diversity. Molecular identification tools, like DNA barcoding, have been successfully used to identify marine planktonic specimens to a species. However, the behaviour of methods for specimen identification and species delimitation remain untested for taxonomically diverse and widely-distributed marine zooplanktonic groups. Using Canadian marine planktonic crustacean collections, I generated a multi-gene data set including COI-5P and 18S-V4 molecular markers of morphologically-identified Copepoda and Thecostraca (Multicrustacea: Hexanauplia) species. I used this data set to assess generalities in the genetic divergence patterns and to determine if a barcode gap exists separating interspecific and intraspecific molecular divergences, which can reliably delimit specimens into species. I then used this information to evaluate the North Pacific, Arctic, and North Atlantic biogeography of marine Calanoida (Hexanauplia: Copepoda) plankton. -
Composition and Sources of Near Reef Zooplankton on a Jamaican Forereef Along with Implications for Coral Feeding
Coral Reefs (2004) 23: 263–276 DOI 10.1007/s00338-004-0375-0 REPORT K. B. Heidelberg Æ K. P. Sebens Æ J. E. Purcell Composition and sources of near reef zooplankton on a Jamaican forereef along with implications for coral feeding Received: 20 September 2001 / Accepted: 17 April 2003 / Published online: 10 March 2004 Ó Springer-Verlag 2004 Abstract Nocturnal near-reef zooplankton from the Keywords Demersal zooplankton Æ Coral feeding Æ forereef of Discovery Bay, Jamaica, were sampled dur- Copepod Æ Reef ing winter and summer 1994 using a diver-operated plankton pump with an intake head positioned within centimeters of benthic zooplanktivores. The pump col- lected zooplankton not effectively sampled by conven- Introduction tional net tows or demersal traps. We found consistently greater densities of zooplankton than did earlier studies Coral reef zooplankton are an important trophic link that used other sampling methods in similar locations. between primary producers and higher trophic levels on There was no significant difference between winter reefs, including scleractinian corals and fish (Porter (3491±578 mÀ3) and summer (2853±293 mÀ3)zoo- 1974; Hobson and Chess 1978; Gottfried and Roman plankton densities. Both oceanic- and reef-associated 1983; Hamner et al. 1988; Sedberry and Cuellar 1993). forms were found at temporal and spatial scales relevant Zooplankton that are potential prey to benthic organ- to benthic suspension feeders. Copepods were always the isms come from several sources and include holoplank- most abundant group, averaging 89% of the total zoo- tonic, meroplanktonic, demersal, and epibenthic species plankton, and most were not of demersal origin. -
Midwater Data Sheet
MIDWATER TRAWL DATA SHEET RESEARCH VESSEL__________________________________(1/20/2013Version*) CLASS__________________;DATE_____________;NAME:_________________________; DEVICE DETAILS___________ LOCATION (OVERBOARD): LAT_______________________; LONG___________________________ LOCATION (AT DEPTH): LAT_______________________; LONG______________________________ LOCATION (START UP): LAT_______________________; LONG______________________________ LOCATION (ONBOARD): LAT_______________________; LONG______________________________ BOTTOM DEPTH_________; DEPTH OF SAMPLE:____________; DURATION OF TRAWL___________; TIME: IN_________AT DEPTH________START UP__________SURFACE_________ SHIP SPEED__________; WEATHER__________________; SEA STATE_________________; AIR TEMP______________ SURFACE TEMP__________; PHYS. OCE. NOTES______________________; NOTES_____________________________ INVERTEBRATES Lensia hostile_______________________ PHYLUM RADIOLARIA Lensia havock______________________ Family Tuscaroridae “Round yellow ones”___ Family Hippopodiidae Vogtia sp.___________________________ PHYLUM CTENOPHORA Family Prayidae Subfamily Nectopyramidinae Class Nuda "Pointed siphonophores"________________ Order Beroida Nectadamas sp._______________________ Family Beroidae Nectopyramis sp.______________________ Beroe abyssicola_____________________ Family Prayidae Beroe forskalii________________________ Subfamily Prayinae Beroe cucumis _______________________ Craseoa lathetica_____________________ Class Tentaculata Desmophyes annectens_________________ Subclass -
CNIDARIA Corals, Medusae, Hydroids, Myxozoans
FOUR Phylum CNIDARIA corals, medusae, hydroids, myxozoans STEPHEN D. CAIRNS, LISA-ANN GERSHWIN, FRED J. BROOK, PHILIP PUGH, ELLIOT W. Dawson, OscaR OcaÑA V., WILLEM VERvooRT, GARY WILLIAMS, JEANETTE E. Watson, DENNIS M. OPREsko, PETER SCHUCHERT, P. MICHAEL HINE, DENNIS P. GORDON, HAMISH J. CAMPBELL, ANTHONY J. WRIGHT, JUAN A. SÁNCHEZ, DAPHNE G. FAUTIN his ancient phylum of mostly marine organisms is best known for its contribution to geomorphological features, forming thousands of square Tkilometres of coral reefs in warm tropical waters. Their fossil remains contribute to some limestones. Cnidarians are also significant components of the plankton, where large medusae – popularly called jellyfish – and colonial forms like Portuguese man-of-war and stringy siphonophores prey on other organisms including small fish. Some of these species are justly feared by humans for their stings, which in some cases can be fatal. Certainly, most New Zealanders will have encountered cnidarians when rambling along beaches and fossicking in rock pools where sea anemones and diminutive bushy hydroids abound. In New Zealand’s fiords and in deeper water on seamounts, black corals and branching gorgonians can form veritable trees five metres high or more. In contrast, inland inhabitants of continental landmasses who have never, or rarely, seen an ocean or visited a seashore can hardly be impressed with the Cnidaria as a phylum – freshwater cnidarians are relatively few, restricted to tiny hydras, the branching hydroid Cordylophora, and rare medusae. Worldwide, there are about 10,000 described species, with perhaps half as many again undescribed. All cnidarians have nettle cells known as nematocysts (or cnidae – from the Greek, knide, a nettle), extraordinarily complex structures that are effectively invaginated coiled tubes within a cell. -
Piggybacking Pycnogonids and Parasitic Narcomedusae on Pandea Rubra (Anthomedusae, Pandeidae)
Plankton Benthos Res 2(2): 83–90, 2007 Plankton & Benthos Research © The Plankton Society of Japan Piggybacking pycnogonids and parasitic narcomedusae on Pandea rubra (Anthomedusae, Pandeidae) FRANCESC PAGÈS1†, JORDI CORBERA2 &DHUGAL LINDSAY3* 1 Institut de Ciències del Mar (CSIC), Passeig Marítim de la Barceloneta 37–49, 08003, Barcelona, Catalunya, Spain 2 Carrer Gran 90, 08310 Argentona, Catalunya, Spain 3 Marine Biology and Ecology Research Program, Extremobiosphere Research Center, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2–15 Natushima-cho, Yokosuka, 237–0061, Japan †Deceased Received 26 October 2006; Accepted 30 January 2007 Abstract: Associations between pycnogonids and the mesopelagic anthomedusan Pandea rubra are reported from two in situ video footage records off the Pacific coast of northern Japan, and from a plankton sample collected in the Weddell Sea (one juvenile of the pycnogonid Pallenopsis (Bathypallenopsis) tritonis). This is the first pelagic record of a pycnogonid in the Southern Ocean and the first record of an association between pycnogonids and a hydroidomedusa at mesopelagic depths. Taxonomic descriptions of both host and associate are given. Two early stages of a parasitic nar- comedusa adhered to the medusan subumbrella are also reported. Possible origins for the pycnogonid-medusa associa- tion are postulated. Key words: Antarctica, anthomedusa, association, Japan, mesopelagic, pycnogonid Hedgpeth (1962) suggested that bathypelagic pycnogo- Introduction nids are parasites or commensals upon larger organisms, Pycnogonids are marine arthropods that are usually ben- possibly medusae, as previous observations had shown that thic in habitat. However, occasionally they are observed the larval stages of pycnogonids can be parasitic on hy- swimming in coastal surface waters (Clark & Carpenter droidomedusae in coastal waters (Lebour 1916, Oshima 1977) or are found in plankton samples collected in upper 1933, Okuda 1940). -
Diel Cycles of Molting, Mating, Egg Sac Production and Hatching in the Swarm Forming Cyclopoid Copepod Dioithona Oculata
Plankton Biol. Ecol. 46 (2): 120-127, 1999 plankton biology & ecology '>"> The IMankion Socicly of Jap;in I'WJ Diel cycles of molting, mating, egg sac production and hatching in the swarm forming cyclopoid copepod Dioithona oculata Julie W. Ambler1, Frank D. Ferrari2, John A. Fornshell2 & Edward J. Buskey3 ' Department of Biology, Millersville University, Millersville. Pennsylvania 17551, U.S.A. : Department of Invertebrate Zoology, Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560, U.S.A. JMarine Science Institute, The University of Texas at Austin, 750 Channelview Drive, Port Aransas, Texas 78373. U.S.A. Received 8 December 1998; accepted 14 June 1999 Abstract: Diel periodicity was discovered in 4 life cycle events for the swarming cyclopoid copepod Dioithona oculata: the molt to adult stage, mating, egg sac production, and egg hatching. The timing of these events was associated with swarming in which dioithonans form swarms at dawn and dis perse at dusk. A laboratory time course experiment revealed that molting of copepodid stage five (CV) to adult (CVI) occurred between midnight and dawn (0600 h). In videotaped experiments of labo ratory swarms, mating encounters were greatest at dawn and therefore would occur as soon as CV molted to adults and were present in swarms. In experiments with field collected swarms, 80% of egg sacs were produced by females between midnight and 0820 h the next morning, and 80% of the eggs hatched by the following night between midnight and 0500 h. Egg cycle duration (clutch duration plus inter-clutch interval) was 48 h, and the mean fecundity was 0.56 pairs of egg sacs d 1 or 7.6 eggs d~1.