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MEDDELELSER NR. 120 IAN GJERTZ & BERIT MØRKVED Environmental Studies from Franz Josef Land, with Emphasis on Tikhaia Bay, Hooker Island '-,.J��!c �"'oo..--------' MikhalSkakuj NORSK POLARINSTITUTT OSLO 1992 ISBN 82-7666-043-6 lan Gjertz and Berit Mørkved Printed J uly 1992 Norsk Polarinstitutt Cover picture: Postboks 158 Iceberg of Franz Josef Land N-1330 Oslo Lufthavn (Ian Gjertz) Norway INTRODUCTION The Russian high Arctic archipelago Franz Josef Land has long been closed to foreign scientists. The political changes which occurred in the former Soviet Union in the last part of the 1980s resulted in the opening of this area to foreigners. Director Gennady Matishov of Murmansk Marine Biological Institute deserves much of the credit for this. In 1990 an international cooperation was established between the Murmansk Marine Biological Institute (MMBI); the Arctic Ecology Group of the Institute of Oceanology, Gdansk; and the Norwegian Polar Research Institute, Oslo. The purpose of this cooperation is to develope scientific cooperation in the Arctic thorugh joint expeditions, the establishment of a high Arctic scientific station, and the exchange of scientific information. So far the results of this cooperation are two scientific cruises with the RV "Pomor", a vessel belonging to the MMBI. The cruises have been named Sov Nor-Poll and Sov-Nor-Po12. A third cruise is planned for August-September 1992. In addition the MMBI has undertaken to establish a scientific station at Tikhaia Bay on Hooker Island. This is the site of a former Soviet meteorological base from 1929-1958, and some of the buildings are now being restored by MMBI. -
Calanus Helgolandicus Under Controlled Conditions
Helgol~inder wiss. Meeresunters. 20, 346-359 (1970) Cultivation of Calanus helgolandicus under controlled conditions G.-A. PAFFENH6FER Institute of Marine Resources, University of California, San Diego; La Jolla, California, USA KURZFASSUNG: Kultlvierung von Calanus helgolandicus unter kontrollierten Bedingungen. Der planktonische Copepode Calanus helgolandicus (Calanoida) wurde im Labor vom Ei bis zum Adultus in bewegten Kulturen bei 15.0 C aufgezogen. Die kettenbildenden Diatomeen Chaetoceros curvisetus, Skeletonema costatum und Lauderia borealis sowie der Dinoflagellat Gymnodinium splendens wurden als Nahrung angeboten. Die Nahrungskonzentrationen, die zum Tell den Phytoplanktonkonzentrationen im Pazifischen Ozean an der Ktiste Siidkalifor- niens entsprachen, lagen zwischen 28 ~g und 800 #g organischem C/I. In Abh~ingigkeit yon Nahrungsquallt~it und Nahrungskonzentration wurden folgende Ergebnisse erzielt: Die Mor- talit~it yon C. heIgolandicus w~.hrend der gesamten Entwicklung vom geschliipf~en Naupllus bis zum Adultus lag zwischen 2,3 °/0 und 58,2 o/0. Die Zeitspanne yore Schliipfen bis zum adul- ten Stadium wiihrte i8 bis 54 Tage. Das Geschlechterverh~imis in verschiedenen KuIturen im Labor aufgezogener Tiere schwankte erhebli&. Der h6chste Prozentsatz yon ~ (~ (ca. 25 %) wurde erhalten, als L. boreal# beziehungswelse G. splendens gef~ittert wurden. Die L~.nge der ~ stand in direktem Verh~ilmis zur angebotenen Nahrungsmenge und lag zwischen 3,03 mm und 3,84 ram. Im Labor aufgezogene mad befruchtete ~ legten durchschnittlich 1991 Eier pro ~ bei einer Schlilpfrate yon 84 °/0. Spermatophorentragende ~ aus dem Pazifischen Ozean legten durchschnittllch je 2267 Eier, die eine Schltipfrate yon 77 % aufwiesen. Die Er- gebnisse beweisen, dab es m/Sglich ist, Calanus helgolandicus ohne Schwierlgkeit im Labor auf- zuziehen. -
Egg Production Rates of the Copepod Calanus Marshallae in Relation To
Egg production rates of the copepod Calanus marshallae in relation to seasonal and interannual variations in microplankton biomass and species composition in the coastal upwelling zone off Oregon, USA Peterson, W. T., & Du, X. (2015). Egg production rates of the copepod Calanus marshallae in relation to seasonal and interannual variations in microplankton biomass and species composition in the coastal upwelling zone off Oregon, USA. Progress in Oceanography, 138, 32-44. doi:10.1016/j.pocean.2015.09.007 10.1016/j.pocean.2015.09.007 Elsevier Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Progress in Oceanography 138 (2015) 32–44 Contents lists available at ScienceDirect Progress in Oceanography journal homepage: www.elsevier.com/locate/pocean Egg production rates of the copepod Calanus marshallae in relation to seasonal and interannual variations in microplankton biomass and species composition in the coastal upwelling zone off Oregon, USA ⇑ William T. Peterson a, , Xiuning Du b a NOAA-Fisheries, Northwest Fisheries Science Center, Hatfield Marine Science Center, Newport, OR, United States b Cooperative Institute for Marine Resources Studies, Oregon State University, Hatfield Marine Science Center, Newport, OR, United States article info abstract Article history: In this study, we assessed trophic interactions between microplankton and copepods by studying Received 15 May 2015 the functional response of egg production rates (EPR; eggs femaleÀ1 dayÀ1) of the copepod Calanus Received in revised form 1 August 2015 marshallae to variations in microplankton biomass, species composition and community structure. Accepted 17 September 2015 Female C. marshallae and phytoplankton water samples were collected biweekly at an inner-shelf station Available online 5 October 2015 off Newport, Oregon USA for four years, 2011–2014, during which a total of 1213 female C. -
Evolutionary History of Inversions in the Direction of Architecture-Driven
bioRxiv preprint doi: https://doi.org/10.1101/2020.05.09.085712; this version posted May 10, 2020. 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-NC 4.0 International license. Evolutionary history of inversions in the direction of architecture- driven mutational pressures in crustacean mitochondrial genomes Dong Zhang1,2, Hong Zou1, Jin Zhang3, Gui-Tang Wang1,2*, Ivan Jakovlić3* 1 Key Laboratory of Aquaculture Disease Control, Ministry of Agriculture, and State Key Laboratory of Freshwater Ecology and Biotechnology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China. 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 Bio-Transduction Lab, Wuhan 430075, China * Corresponding authors Short title: Evolutionary history of ORI events in crustaceans Abbreviations: CR: control region, RO: replication of origin, ROI: inversion of the replication of origin, D-I skew: double-inverted skew, LBA: long-branch attraction bioRxiv preprint doi: https://doi.org/10.1101/2020.05.09.085712; this version posted May 10, 2020. 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-NC 4.0 International license. Abstract Inversions of the origin of replication (ORI) of mitochondrial genomes produce asymmetrical mutational pressures that can cause artefactual clustering in phylogenetic analyses. It is therefore an absolute prerequisite for all molecular evolution studies that use mitochondrial data to account for ORI events in the evolutionary history of their dataset. -
A Systematic and Experimental Analysis of Their Genes, Genomes, Mrnas and Proteins; and Perspective to Next Generation Sequencing
Crustaceana 92 (10) 1169-1205 CRUSTACEAN VITELLOGENIN: A SYSTEMATIC AND EXPERIMENTAL ANALYSIS OF THEIR GENES, GENOMES, MRNAS AND PROTEINS; AND PERSPECTIVE TO NEXT GENERATION SEQUENCING BY STEPHANIE JIMENEZ-GUTIERREZ1), CRISTIAN E. CADENA-CABALLERO2), CARLOS BARRIOS-HERNANDEZ3), RAUL PEREZ-GONZALEZ1), FRANCISCO MARTINEZ-PEREZ2,3) and LAURA R. JIMENEZ-GUTIERREZ1,5) 1) Sea Science Faculty, Sinaloa Autonomous University, Mazatlan, Sinaloa, 82000, Mexico 2) Coelomate Genomic Laboratory, Microbiology and Genetics Group, Industrial University of Santander, Bucaramanga, 680007, Colombia 3) Advanced Computing and a Large Scale Group, Industrial University of Santander, Bucaramanga, 680007, Colombia 4) Catedra-CONACYT, National Council for Science and Technology, CDMX, 03940, Mexico ABSTRACT Crustacean vitellogenesis is a process that involves Vitellin, produced via endoproteolysis of its precursor, which is designated as Vitellogenin (Vtg). The Vtg gene, mRNA and protein regulation involve several environmental factors and physiological processes, including gonadal maturation and moult stages, among others. Once the Vtg gene, mRNAs and protein are obtained, it is possible to establish the relationship between the elements that participate in their regulation, which could either be species-specific, or tissue-specific. This work is a systematic analysis that compares the similarities and differences of Vtg genes, mRNA and Vtg between the crustacean species reported in databases with respect to that obtained from the transcriptome of Callinectes arcuatus, C. toxotes, Penaeus stylirostris and P. vannamei obtained with MiSeq sequencing technology from Illumina. Those analyses confirm that the Vtg obtained from selected species will serve to understand the process of vitellogenesis in crustaceans that is important for fisheries and aquaculture. RESUMEN La vitelogénesis de los crustáceos es un proceso que involucra la vitelina, producida a través de la endoproteólisis de su precursor llamado Vitelogenina (Vtg). -
How Including Ecological Realism Impacts the Assessment of the Environmental Effect of Oil Spills at the Population Level: the A
How including ecological realism impacts the assessment of the environmental effect of oil spills at the population level: The application of matrix models for Arctic Calanus species de Vries, P., Tamis, J., Hjorth, M., Jak, R., Falk-Petersen, S., van den Heuvel- Greve, M., ... Hemerik, L. This is a "Post-Print" accepted manuscript, which has been published in "Marine Environmental Research" This version is distributed under a non-commercial no derivatives Creative Commons (CC-BY-NC-ND) user license, which permits use, distribution, and reproduction in any medium, provided the original work is properly cited and not used for commercial purposes. Further, the restriction applies that if you remix, transform, or build upon the material, you may not distribute the modified material. Please cite this publication as follows: de Vries, P., Tamis, J., Hjorth, M., Jak, R., Falk-Petersen, S., van den Heuvel-Greve, M., ... Hemerik, L. (2018). How including ecological realism impacts the assessment of the environmental effect of oil spills at the population level: The application of matrix models for Arctic Calanus species. Marine Environmental Research, 141, 264- 274. DOI: 10.1016/j.marenvres.2018.09.008 You can download the published version at: https://doi.org/10.1016/j.marenvres.2018.09.008 Accepted Manuscript How including ecological realism impacts the assessment of the environmental effect of oil spills at the population level: The application of matrix models for Arctic Calanus species Pepijn de Vries, Jacqueline Tamis, Morten Hjorth, Robbert -
Hidden Food in the Coldest of Times the NUTRIENT ROLE of SEA ICE Copepods, Tiny Lipid-Rich Obtaining Sufficient Food Under Fig
UNDERSTANDING ECOSYSTEM PROCESSES IN THE BERING SEA 2007–2013 Hidden Food in the Coldest of Times THE NUTRIENT ROLE OF SEA ICE Copepods, tiny lipid-rich obtaining sufficient food under Fig. 1 crustaceans in the Bering Sea, the ice to initiate feeding and are a favored meal of larval and reproduction. A second question juvenile Pollock. One copepod is “what is this food source”? One that dominates the zooplankton possibility was the layer of ice on the Bering Sea shelf, and shelf algae—a diverse community of areas around the Arctic Ocean, microscopic plants and animals is Calanus glacialis (Figure 1). that grow under the ice during We know that the abundance of spring (Figure 2)—rather than this species fluctuates between from the more usual phytoplank- years. Surprisingly, colder years, ton community in the water when ice cover is more extensive column beneath. and persists longer during spring, appear to favor growth of the How We Did It copepod population. Why is this? We collected zooplankton We set out to answer this ques- samples to see what the C. glacialis Fig. 2 tion during a cruise in late winter population was doing, whether of 2009 through early spring of the adult females were laying eggs 2010, when ice covered most of or not, and how much food was the Bering Sea shelf. in their guts. We determined the Since reproduction and identity of individual prey spe- growth of this copepod is con- cies in their guts from their DNA trolled by the availability of food, and quantified the amount of this we thought that they must be continued on page 2 The Big Picture The high feeding rates of the copepod Calanus glacialis that we observed during a cruise in late Blocks of sea ice turned winter and early spring of 2009/2010 could not have been sustained by the low levels of phyto- upside down to reveal plankton in the water column. -
Canada's Arctic Marine Atlas
CANADA’S ARCTIC MARINE ATLAS This Atlas is funded in part by the Gordon and Betty Moore Foundation. I | Suggested Citation: Oceans North Conservation Society, World Wildlife Fund Canada, and Ducks Unlimited Canada. (2018). Canada’s Arctic Marine Atlas. Ottawa, Ontario: Oceans North Conservation Society. Cover image: Shaded Relief Map of Canada’s Arctic by Jeremy Davies Inside cover: Topographic relief of the Canadian Arctic This work is licensed under the Creative Commons Attribution-NonCommercial 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/4.0 or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. All photographs © by the photographers ISBN: 978-1-7752749-0-2 (print version) ISBN: 978-1-7752749-1-9 (digital version) Library and Archives Canada Printed in Canada, February 2018 100% Carbon Neutral Print by Hemlock Printers © 1986 Panda symbol WWF-World Wide Fund For Nature (also known as World Wildlife Fund). ® “WWF” is a WWF Registered Trademark. Background Image: Phytoplankton— The foundation of the oceanic food chain. (photo: NOAA MESA Project) BOTTOM OF THE FOOD WEB The diatom, Nitzschia frigida, is a common type of phytoplankton that lives in Arctic sea ice. PHYTOPLANKTON Natural history BOTTOM OF THE Introduction Cultural significance Marine phytoplankton are single-celled organisms that grow and develop in the upper water column of oceans and in polar FOOD WEB The species that make up the base of the marine food Seasonal blooms of phytoplankton serve to con- sea ice. Phytoplankton are responsible for primary productivity—using the energy of the sun and transforming it via pho- web and those that create important seafloor habitat centrate birds, fishes, and marine mammals in key areas, tosynthesis. -
Fractal Distribution of an Oceanic Copepod Neocalanus Cristatus in the Subarctic Pacific
Journal of Oceanography Vol. 51, pp. 261 to 266. 1995 Fractal Distribution of an Oceanic Copepod Neocalanus cristatus in the Subarctic Pacific ATSUSHI TSUDA Ocean Research Institute, University of Tokyo 1-15-1, Minamidai, Nakano, Tokyo 164, Japan (Received 13 April 1994; in revised form 28 June 1994; accepted 30 August 1994) Horizontal distribution of the copepod Neocalanus cristatus was shown to be fractal on the scale between tens of meters and over 100 km. The fractal dimensions ranged between 1.68–1.89, significantly higher than those of oceanic turbulence and phytoplankton distribution. 1. Introduction Heterogeneity in the horizontal distribution of zooplankton has been recognized for many years (e.g. Hardy, 1936). The phenomenon, however, has seldom been described precisely, although zooplankton patchiness is relevant to many aspects of biological oceanography. Recent studies reveal that copepod patches do not exhibit characteristic lengths (Mackas and Boyd, 1979; Tsuda et al., 1993) and that the patterns of copepod distribution are self-similar and independent of the scale of observation (Tsuda et al., 1993). These findings suggest that copepod distributions may be fractal. Mandelbrot (1967) introduced the concept of fractals for temporally or spatially irregular phenomena which show self-similarities over a wide range of scales. Many fractal objects have been found in nature (Mandelbrot, 1982), and the theory has been applied to some ecological studies (Morse et al., 1985; Pennycuick and Kline, 1986; Dicke and Burrough, 1988; Sugihara and May, 1990; McKinney and Frederick, 1992). In the oceans, environmental turbulence itself has fractal facets in many aspects (Mandelbrot, 1982; Sreenivasan and Meneveau, 1986). -
Foraging Radii and Energetics of Least Auklets (Aethia Pusilla) Breeding on Three Bering Sea Islands
647 Foraging Radii and Energetics of Least Auklets (Aethia pusilla) Breeding on Three Bering Sea Islands Bryan S. Obst1·* Robert W. Russell2·t 2 George L. Hunt, Jr. ·; Zoe A. Eppler·§ Nancy M. Harrison2·ll 1Departmem of Biology, University of California, Los Angeles, California 90024; 2Depanment of Ecology and Evolutionary Biology, University of California, Irvine, California 92717 Accepted 11/18/94 Abstract We studied the relationship between the foraging radius and energy economy of least auklets (Aethia pusilla) breeding in colonies on three islands in the Bering Sea (St. Lawrence, St. Matthew, and St. George Islands). The distan:ce to which auklets commuted on foraging trips varied by more than an order of magnitude (5-56 km), but mean field metabolic rate (FMR) did not vary significantly among birds from the three islands. These observations indicate that allocation to various compartments of time and energy budgets is flexible and suggest that least auklets may have a preferred level ofdaily energy expenditure that is simi lar across colonies. We modeled the partitioning of energy to various activities and hypothesize that the added cost of commuting incurred by auktets from St. Lawrence Island (foraging radius, 56 km) was offiet by reduced energy costs while foraging at sea. Data on bird diets and prey abundances indicated that aukletsfrom St. Lawrence Island fed on larger, more energy-rich copepods than did aukletsfrom St. Matthew island (foraging radius, 5 km) but that depth-aver aged prey density did not differ significantly between the birds' principal forag ing areas. However, previous studies have indicated that zooplankton abun dance is vertically compressed into near-surface layers in stratified waters off St. -
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. -
Life Cycle and Distribution of Calanus Finmarchicus in Deep Basins on the Nova Scotia Shelf and Seasonal Changes in Calanus Spp
MARINE ECOLOGY PROGRESS SERIES Vol. 66: 225-237, 1990 Published September 6 Mar. Ecol. Prog. Ser. Life cycle and distribution of Calanus finmarchicus in deep basins on the Nova Scotia shelf and seasonal changes in Calanus spp. ' Biological Sciences Branch, Department of Fisheries and Oceans. Bedford Institute of Oceanography, PO Box 1006, Dartmouth, Nova Scotia, Canada B2Y 4A2 Physical/Chemical Sciences Branch, Department of Fisheries and Oceans. Bedford Institute of Oceanography, PO Box 1006, Dartmouth. Nova Scotia. Canada B2Y 4A2 ABSTRACT: The deep basins on the Nova Scotia shelf contain high concentrations of Calanus finmarchicus, C. glacialis, and C. hyperboreus at depths below 200 m. From May to late fall these were as high as 20 000 m-3. The dominant specles by numbers was C. finmarchicus; however, its biomass was equalled or exceeded by C. hyperboreus. The life cycle of C. finmarchicus in the region of 2 of the largest basins showed that breeding started late in winter with a peak in April. High concentrations of Calanus suggested that the basins had higher levels of C. finmarchicus production than the adjacent shelf with mean depths less than 100 m. All 3 species of Calanus started to accumulate below 200 m in May as Stages CIV and CV C. glacialisand C. hyperboreusdid not reproduce in significant numbers on the NW half of the shelf but did accumulate in the basins as they were advected from the NE shelf region. Resting stages of Calanus resided at depths below 200 m in water at between 8.5 and 11 "C for an estimated 7 to 8 mo.