Contaminants in Marine Mammals in Greenland
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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. -
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 -
Tautuglugu Uvani PDF Mi Makpiraanmi
KANATAUP UKIUQTAQTUNGATA TARIURMIUTANUT NUNANNGUAQ Taanna Nunannguaq kiinaujaqaqtitaujuq ilangani Gordon amma Betty Moore Katujjiqatigiinik. I | Atuqujaujuq takujaujunnarluni: Tariurjualirijikkut Ukiuqtaqtumi Atutsiarnirmut Katujjiqatigiit, Nunarjuarmi Uumajulirijikkut Kiinajangit Kanatami, amma Mitilirijikkut Kanatami. (2018). Kanataup Ukiuqtaqtungata Tariurmiutanut Nunannguaq. Aatuvaa, Antiariu: Tariurjualirijikkut Ukiuqtaqtumi Atutsiarnirmut Katujjiqatigiit. Qaangata ajjinnguanga: Siarnaulluni Nunannguaq Kanataup Ukiuqtaqtungani taassuma Jeremy Davies Iluaniittuq: Nalunaijaqsimattiaqtuq Kanataup Ukiuqtaqtungani Tamanna piliriangujuq laisansiqaqtuq taakuatigut Creative Commons Attribution-NonCommercial 4.0 Nunarjuarmi Laisansi. Taasumaa laisansimi takugumaguvit, uvungarluti http://creativecommons.org/licenses/by-nc/4.0 uvvaluunniit uvunga titirarlutit Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. Ajjinngualimaat © ajjiliurijinut Naasautinga (ISBN): 978-1-7752749-0-2 (paippaamut saqqititat) Naasautinga (ISBN): 978-1-7752749-1-9 (qarasaujatigut saqqititat) Uqalimaagaqarvik amma Tuqquqtausimavik Kanatami AJJIGIINNGITTUT Paippaat kamattiaqtuninngaaqsimajut Paippaarmuuqtajut Kanatami, Vivvuali 2018 100% Pauqititsijunnanngittuq Saqqititaq taassuma Hemlock Saqqititsijikkunnu © 1986 Paannti nalunaikkutaq WWF-Nunarjualimaami Kinaujaqarvik Uumajunut (qaujimajaungmijuq Nunarjualimaamit Uumajunut Kinaujaqarvik). ® “WWF” taanaujuq WWF Atiliuqatausimajuq Ilisarijaulluni. Tunuaniittuq Ajjinnguanga: Imarmiutait piruqtut attatiqanngittut -
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. -
WILD GREENLAND ESCAPE Current Route: Kangerlussuaq, Greenland to Kangerlussuaq, Greenland
WILD GREENLAND ESCAPE Current route: Kangerlussuaq, Greenland to Kangerlussuaq, Greenland 6 Days National Geographic Resolution 126 Guests Expeditions in: Jul From $8,220 to $16,450 * Call us at 1.800.397.3348 or call your Travel Agent. In Australia, call 1300.361.012 • www.expeditions.com DAY 1: Kangerlussuaq, Greenland padding Fly by chartered aircraft to Kangerlussuaq on 2022 Departure Dates: Greenland’s western coast. Settle into your cabin aboard National Geographic Resolution, the 7 Jul, 12 Jul newest ship in the fleet. (L,D) Advance Payment: DAY 2: Greenland’s West Coast & Sisimiut $1,000 padding Cruise the length of Kangerlussuaq Fjord en route to Sisimiut. Dozens of deep fjords carve into Greenland’s west coast, many with glaciers fed by the ice cap that covers 80 percent of the country. At Sisimiut, a former whaling port, visit the museum and wander amid a jumble of 18th- century wooden buildings. There are several walking options to explore in and around town. (B,L,D) DAY 3: Ilulissat & Disko Bay padding Sail into Disko Bay and set out to explore a tongue of the Greenland ice cap. Take an extraordinary cruise among towering icebergs of the UNESCO World Heritage-designated Ilulissat Icefjord. Visit the town of Ilulissat and take a hike to an archaeological site in the Sermermiut Valley. As we make our way north through Disko Bay, if ice conditions permit, follow the inside passage of Disko Island and continue to Nuussuaq Peninsula. (B,L,D) DAY 4: Uummannaq / Qilakitsoq padding The village of Uummannaq sits on a tiny island in the Uummannaq Fjord that is dominated by a massive peak that rises dramatically at its center. -
Marine Ecology Progress Series 555:49
CORE Metadata, citation and similar papers at core.ac.uk Provided by Brage Nord Open Research Archive Vol. 555: 49–64, 2016 MARINE ECOLOGY PROGRESS SERIES Published August 18 doi: 10.3354/meps11831 Mar Ecol Prog Ser OPENPEN ACCESSCCESS Seasonal vertical strategies in a high-Arctic coastal zooplankton community Kanchana Bandara1,*, Øystein Varpe2,3, Janne E. Søreide2, Jago Wallenschus2, Jørgen Berge2,4, Ketil Eiane1 1Faculty of Biosciences and Aquaculture, Nord University, 8049 Bodø, Norway 2The University Centre in Svalbard (UNIS), 9171 Longyearbyen, Norway 3Akvaplan-niva, Fram Centre, 9296 Tromsø, Norway 4Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, 9037 Tromsø, Norway ABSTRACT: We studied the larger (>1000 µm) size fraction of zooplankton in an Arctic coastal water community in Billefjorden, Svalbard (78°40’ N), Norway, in order to describe seasonal ver- tical distributions of the dominant taxa in relation to environmental variability. Calanus spp. numerically dominated the herbivores; Aglantha digitale, Mertensia ovum, Beroë cucumis, and Parasagitta elegans were the dominant carnivores. Omnivores and detritivores were numerically less important. Descent to deeper regions of the water column (>100 m) between August and October, and ascent to the shallower region (<100 m) between November and May was the overall seasonal pattern in this zooplankton community. In contrast to other groups, P. elegans did not exhibit pronounced vertical migrations. Seasonal vertical distributions of most species showed statistical associations with the availability of their main food source. The vertical distribution of later developmental stages of Calanus spp. was inversely associated with fluorescence, indicating that they descended from the shallower region while it was still relatively productive, and ascended before the primary production had started to increase. -
Arctic & Greenland Expedition Cruise
REYKJAVIK TO CHURCHILL: ARCTIC & GREENLAND EXPEDITION CRUISE Join us for a journey that follows the route of the Norse in their explorations of Greenland. Heading first to East Greenland, we will experience the beauty of deep fjords and crystal clear glaciers. In South and West Greenland, we will see the remains of Norse settlements and will visit small towns and villages to encounter a fascinating mix of local and Danish culture. Heading over to Nunavut we will be looking for polar bears and walrus during Zodiac cruises. We will see outstanding local art in Iqaluit and Cape Dorset and will look for beluga whales in Churchill. Throughout the voyage, learn about the history, geology, wildlife and botany of this spectacular area from lecture presentations offered by your knowledgeable onboard Expedition Team. ITINERARY Day 1 REYKJAVIK Sprawling Reykjavík, the nation's nerve center and government seat, is home to half the island's population. On a bay overlooked by proud Mt. Esja (pronounced eh-shyuh), with its ever-changing hues, Reykjavík presents a colorful sight, its concrete houses painted in light colors and topped by vibrant red, blue, and green roofs. In contrast to the almost treeless countryside, Reykjavík has many tall, native birches, rowans, and willows, as well as imported aspen, pines, and spruces.Reykjavík's name comes from the Icelandic words for smoke, reykur, and bay, vík. Day 2 DAY AT SEA 01432 507 280 (within UK) [email protected] | small-cruise-ships.com Days at sea are the perfect opportunity to relax, unwind and land in the area around Aapilattoq since the 19th century. -
AGUIDE to Frle DEVELOPMENTAL STAGES of COMMON COASTAL
A GUIDE TO frlE DEVELOPMENTAL STAGES OF COMMON COASTAL, GeORGES BANK AND GULF OF MAINE COPEPODS BY Janet A. Murphy and Rosalind E. Cohen National Marine Fisheries Service Northeast Fisheries Center Woods Hole Laboratory Woods Hole, MA 02543 Laboratory Reference No. 78-53 Table of Contents List of Plates i,,;i,i;i Introduction '. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 1 Acarti a cl aus; .. 2 Aca rtia ton sa .. 3 Aca rtia danae .. 4 Acartia long; rem; s co e"" 5 Aetidi us artllatus .. 6 A1teutha depr-e-s-s-a· .. 7 Calanu5 finmarchicus .............•............................ 8 Calanus helgolandicus ~ 9 Calanus hyperboreus 10 Calanus tenuicornis .......................•................... 11 Cal oca 1anus pavo .....................•....•....•.............. 12 Candaci a armata Ii II .. .. .. .. .. .. .. .. .. .. 13 Centropages bradyi............................................ 14 Centropages hama tus .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 15 ~ Centropages typi cus " .. " 0 16 Clausocalanus arcuicornis ..............................•..•... 17 Clytemnestra rostra~ta ................................•.•........ 18 Corycaeus speciosus........................................... 19 Eucalanus elongatu5 20 Euchaeta mar; na " . 21 Euchaeta norveg; ca III co .. 22 Euchirel1a rostrata . 23 Eurytemora ameri cana .......................................•.. 24 Eurytemora herdmani , . 25 Eurytemora hi rundoi des . 26 Halithalestris croni ..................•...................... -
Measured and Inferred Gross Energy Content in Diapausing Calanus Spp
JOURNAL OF PLANKTON RESEARCH j VOLUME 34 j NUMBER 7 j PAGES 614–625 j 2012 Measured and inferred gross energy content in diapausing Calanus spp. in a Scotian shelf basin KIMBERLEY T. A. DAVIES*, AMY RYAN AND CHRISTOPHER T. TAGGART DEPARTMENT OF OCEANOGRAPHY, DALHOUSIE UNIVERSITY, 1355 OXFORD STREET, PO BOX 15000, HALIFAX, NS, CANADA B3H4R2 *CORRESPONDING AUTHOR: [email protected] Downloaded from Received December 23, 2011; accepted in principle March 19, 2012; accepted for publication March 23, 2012 Corresponding editor: Roger Harris Calanus finmarchicus stage-C5 and C. hyperboreus stage-C4 diapausing in Scotian Shelf http://plankt.oxfordjournals.org/ basins are high-quality food sources because they are abundant and high in energy content. When combined, these two variables are informative for quantify- ing energy density, carrying capacity and energy transfer in marine ecosystems. However, measuring energy content directly can be difficult and expensive. Here, we present energy (caloric) content estimates for two co-located diapausing copepod species; C. finmarchicus C5 and C. hyperboreus C4 collected during late- summer when their energy content is at or near the annual maximum. We then develop several practical energy content calibrations, each designed to estimate energy content using simple measures of Calanus spp. body size or weight. Weight- at Dalhousie University on July 24, 2012 specific energy content (energy quality, kJ g21) did not differ between C. finmarchi- cus and C. hyperboreus; i.e. body size explained the majority of inter-species variation in individual energy content (J ind.21). Energy content estimated directly using calorimetry did not differ from energy inferred from oil sac volume (OSV), demonstrating that energy content can be inferred when direct energy estimates are unavailable. -
Canada's Arctic Marine Atlas
Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baffin e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baffin Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King -
Dartmouth Wild Greenland Escape Brochure
WILD GREENLAND ESCAPE 6 DAYS/5 NIGHTS | ABOARD NATIONAL GEOGRAPHIC RESOLUTION JULY 12-17, 2022 | TRAVEL WITH PROFESSOR MEREDITH KELLY Venture to the fjord-laced coast of western Greenland, where hardy Inuit communities perched at the edge of the Greenland Uummannaq ice cap carry on their timeless way of life. Qilakitsoq Explore archaeological sites and vibrant Ilulissat modern-day villages, glide into breathtaking Davis Strait fjords by Zodiac or kayak, watch for the GREENLAND Ataneq Northern Lights as we explore the ins and outs of this rugged coastline. Take Sisimiut Kangerlussuaq an unforgettable cruise amid the massive ARCTIC CIRCLE icebergs of the Illulissat Icefjord and meet local people who live off the land and sea as their ancestors before them did for millennia. DAY 1: U.S./Kangerlussuaq, Greenland Fly by chartered aircraft to Kangerlussuaq on Greenland’s western coast. Settle into your cabin aboard National Geographic Resolution, the newest ship in the fleet. (L,D) DAY 2: Greenland’s West Coast & Sisimiut Cruise the length of Kangerlussuaq Fjord en route to Sisimiut. Dozens of deep fjords carve into Greenland’s west coast, many with glaciers fed by the ice cap that covers 80% of the country. At Sisimiut, a former whaling port, visit the museum and wander amid a jumble of wooden 18th-century buildings. There are several walking options to explore in and around town. (B,L,D) DAY 3: Ilulissat & Disko Bay Sail into Disko Bay and set out to explore a tongue of the Greenland ice cap. Take an extraordinary cruise among towering icebergs of the UNESCO World Heritage-designated Ilulissat Icefjord. -
Polish Polar Res. 4-17.Indd
vol. 38, no. 4, pp. 459–484, 2017 doi: 10.1515/popore-2017-0023 Characterisation of large zooplankton sampled with two different gears during midwinter in Rijpfjorden, Svalbard Katarzyna BŁACHOWIAK-SAMOŁYK1*, Adrian ZWOLICKI2, Clare N. WEBSTER3, Rafał BOEHNKE1, Marcin WICHOROWSKI1, Anette WOLD4 and Luiza BIELECKA5 1 Institute of Oceanology Polish Academy of Sciences, Powstańców Warszawy 55, 81-712 Sopot, Poland 2 University of Gdańsk, Department of Vertebrate Ecology and Zoology, Wita Stwosza 59, 80-308 Gdańsk, Poland 3 Pelagic Ecology Research Group, Scottish Oceans Institute, University of St Andrews, KY16 8LB, St Andrews, UK 4 Norwegian Polar Institute, Framsenteret, 9296 Tromsø, Norway 5 Department of Marine Ecosystems Functioning, Faculty of Oceanography and Geography, Institute of Oceanography, University of Gdańsk, Al. Marszałka Piłsudskiego 46, 81-378 Gdynia, Poland * corresponding author <[email protected]> Abstract: During a midwinter cruise north of 80oN to Rijpfjorden, Svalbard, the com- position and vertical distribution of the zooplankton community were studied using two different samplers 1) a vertically hauled multiple plankton sampler (MPS; mouth area 0.25 m², mesh size 200 μm) and 2) a horizontally towed Methot Isaacs Kidd trawl (MIK; mouth area 3.14 m², mesh size 1500 μm). Our results revealed substantially higher species diversity (49 taxa) than if a single sampler (MPS: 38 taxa, MIK: 28) had been used. The youngest stage present (CIII) of Calanus spp. (including C. finmarchi- cus and C. glacialis) was sampled exclusively by the MPS, and the frequency of CIV copepodites in MPS was double that than in MIK samples. In contrast, catches of the CV-CVI copepodites of Calanus spp.