The Laptev Sea Walrus Odobenus Rosmarus Laptevi
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Age-Specific Birth Rates of California Sea Lions
MARINE MAMMAL SCIENCE, 24(3): 664–676 (July 2008) C 2008 by the Society for Marine Mammalogy DOI: 10.1111/j.1748-7692.2008.00199.x Age-specific birth rates of California sea lions (Zalophus californianus) in the Gulf of California, Mexico CLAUDIA J. HERNANDEZ´ -CAMACHO Laboratorio de Ecologıa´ de Pinnıpedos´ “Burney J. Le Boeuf,” Centro Interdisciplinario de Ciencias Marinas, Instituto Politecnico´ Nacional, Ave. IPN s/n Colonia Playa Palo de Santa Rita, La Paz, Baja California Sur, Mexico 23096 and School of Life Sciences, Arizona State University, P. O. Box 874601, Tempe, Arizona 85287-4601, U.S.A. E-mail: [email protected] DAVID AURIOLES-GAMBOA Laboratorio de Ecologıa´ de Pinnıpedos´ “Burney J. Le Boeuf,” Centro Interdisciplinario de Ciencias Marinas, Instituto Politecnico´ Nacional, Ave. IPN s/n Colonia Playa Palo de Santa Rita, La Paz, Baja California Sur, Mexico 23096 LEAH R. GERBER School of Life Sciences, Arizona State University, P. O. Box 874601, Tempe, Arizona 85287-4601, U.S.A. ABSTRACT Estimates of demographic parameters are essential for assessing the status of populations and assigning conservation priority. In light of the difficulties associated with obtaining such estimates, vital rates are rarely available even for well-studied species. We present the first estimates of age-specific birth rates for female California sea lions (Zalophus californianus) >10 yr of age. These rates were estimated from the reproductive histories of five cohorts of animals branded as pups between 1980 and 1984 at Los Islotes colony in the Gulf of California, Mexico. Age-specific birth rates varied among age classes and ranged between 0.06 and 0.80. -
Consensus Statement
Arctic Climate Forum Consensus Statement 2020-2021 Arctic Winter Seasonal Climate Outlook (along with a summary of 2020 Arctic Summer Season) CONTEXT Arctic temperatures continue to warm at more than twice the global mean. Annual surface air temperatures over the last 5 years (2016–2020) in the Arctic (60°–85°N) have been the highest in the time series of observations for 1936-20201. Though the extent of winter sea-ice approached the median of the last 40 years, both the extent and the volume of Arctic sea-ice present in September 2020 were the second lowest since 1979 (with 2012 holding minimum records)2. To support Arctic decision makers in this changing climate, the recently established Arctic Climate Forum (ACF) convened by the Arctic Regional Climate Centre Network (ArcRCC-Network) under the auspices of the World Meteorological Organization (WMO) provides consensus climate outlook statements in May prior to summer thawing and sea-ice break-up, and in October before the winter freezing and the return of sea-ice. The role of the ArcRCC-Network is to foster collaborative regional climate services amongst Arctic meteorological and ice services to synthesize observations, historical trends, forecast models and fill gaps with regional expertise to produce consensus climate statements. These statements include a review of the major climate features of the previous season, and outlooks for the upcoming season for temperature, precipitation and sea-ice. The elements of the consensus statements are presented and discussed at the Arctic Climate Forum (ACF) sessions with both providers and users of climate information in the Arctic twice a year in May and October, the later typically held online. -
Marine Mammals of Hudson Strait the Following Marine Mammals Are Common to Hudson Strait, However, Other Species May Also Be Seen
Marine Mammals of Hudson Strait The following marine mammals are common to Hudson Strait, however, other species may also be seen. It’s possible for marine mammals to venture outside of their common habitats and may be seen elsewhere. Bowhead Whale Length: 13-19 m Appearance: Stocky, with large head. Blue-black body with white markings on the chin, belly and just forward of the tail. No dorsal fin or ridge. Two blow holes, no teeth, has baleen. Behaviour: Blow is V-shaped and bushy, reaching 6 m in height. Often alone but sometimes in groups of 2-10. Habitat: Leads and cracks in pack ice during winter and in open water during summer. Status: Special concern Beluga Whale Length: 4-5 m Appearance: Adults are almost entirely white with a tough dorsal ridge and no dorsal fin. Young are grey. Behaviour: Blow is low and hardly visible. Not much of the body is visible out of the water. Found in small groups, but sometimes hundreds to thousands during annual migrations. Habitat: Found in open water year-round. Prefer shallow coastal water during summer and water near pack ice in winter. Killer Whale Status: Endangered Length: 8-9 m Appearance: Black body with white throat, belly and underside and white spot behind eye. Triangular dorsal fin in the middle of the back. Male dorsal fin can be up to 2 m in high. Behaviour: Blow is tall and column shaped; approximately 4 m in height. Narwhal Typically form groups of 2-25. Length: 4-5 m Habitat: Coastal water and open seas, often in water less than 200 m depth. -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Walrus: Wildlife Notebook Series
Walrus Pacific walruses (Odobenus rosmarus divergens) belong to a group of marine mammals known as pinnipeds (pinna, a wing or fin; and pedis, a foot), this group also includes the seals and sea lions. Walruses are most commonly found in relatively shallow water areas, close to ice or land. In Alaska, their geographic range includes the Bering and Chukchi Seas. General description: Walruses are the largest pinnipeds in arctic and subarctic seas. The genus name Odobenus means “tooth-walker.” Walrus tusks are elongated upper canine teeth both males and females have tusks. Walruses and sea lions can rotate their hind flippers forward to ‘walk’ on them but seals cannot and drag their hind limbs when moving on land or ice. Walruses are large pinnipeds and adult males (bulls) may weigh 2 tons and the females (cows) may exceed 1 ton. Bulls can be identified by their larger size, broad muzzle, heavy tusks, and the presence of numerous large bumps, called bosses, on the neck and shoulders. Food habits: Walruses feed mainly on invertebrates such as clams and snails found on the bottom of the relatively shallow and rich Bering and Chukchi Seas. Walruses find food by brushing the sea-bottom with their broad, flat muzzles using their sensitive whiskers to locate food items. Tusks are not used for finding food. Walruses feed using suction formed by pulling back a thick piston-like tongue inside their narrow mouth. Walruses are able to suck the soft parts out of the shells; few hard parts are ingested. The rejected shells of clams and snails can be found on the sea floor near the furrows made during feeding. -
56. Otariidae and Phocidae
FAUNA of AUSTRALIA 56. OTARIIDAE AND PHOCIDAE JUDITH E. KING 1 Australian Sea-lion–Neophoca cinerea [G. Ross] Southern Elephant Seal–Mirounga leonina [G. Ross] Ross Seal, with pup–Ommatophoca rossii [J. Libke] Australian Sea-lion–Neophoca cinerea [G. Ross] Weddell Seal–Leptonychotes weddellii [P. Shaughnessy] New Zealand Fur-seal–Arctocephalus forsteri [G. Ross] Crab-eater Seal–Lobodon carcinophagus [P. Shaughnessy] 56. OTARIIDAE AND PHOCIDAE DEFINITION AND GENERAL DESCRIPTION Pinnipeds are aquatic carnivores. They differ from other mammals in their streamlined shape, reduction of pinnae and adaptation of both fore and hind feet to form flippers. In the skull, the orbits are enlarged, the lacrimal bones are absent or indistinct and there are never more than three upper and two lower incisors. The cheek teeth are nearly homodont and some conditions of the ear that are very distinctive (Repenning 1972). Both superfamilies of pinnipeds, Phocoidea and Otarioidea, are represented in Australian waters by a number of species (Table 56.1). The various superfamilies and families may be distinguished by important and/or easily observed characters (Table 56.2). King (1983b) provided more detailed lists and references. These and other differences between the above two groups are not regarded as being of great significance, especially as an undoubted fur seal (Australian Fur-seal Arctocephalus pusillus) is as big as some of the sea lions and has some characters of the skull, teeth and behaviour which are rather more like sea lions (Repenning, Peterson & Hubbs 1971; Warneke & Shaughnessy 1985). The Phocoidea includes the single Family Phocidae – the ‘true seals’, distinguished from the Otariidae by the absence of a pinna and by the position of the hind flippers (Fig. -
Sediment Transport to the Laptev Sea-Hydrology and Geochemistry of the Lena River
Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River V. RACHOLD, A. ALABYAN, H.-W. HUBBERTEN, V. N. KOROTAEV and A. A, ZAITSEV Rachold, V., Alabyan, A., Hubberten, H.-W., Korotaev, V. N. & Zaitsev, A. A. 1996: Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River. Polar Research 15(2), 183-196. This study focuses on the fluvial sediment input to the Laptev Sea and concentrates on the hydrology of the Lena basin and the geochemistry of the suspended particulate material. The paper presents data on annual water discharge, sediment transport and seasonal variations of sediment transport. The data are based on daily measurements of hydrometeorological stations and additional analyses of the SPM concentrations carried out during expeditions from 1975 to 1981. Samples of the SPM collected during an expedition in 1994 were analysed for major, trace, and rare earth elements by ICP-OES and ICP-MS. Approximately 700 h3freshwater and 27 x lo6 tons of sediment per year are supplied to the Laptev Sea by Siberian rivers, mainly by the Lena River. Due to the climatic situation of the drainage area, almost the entire material is transported between June and September. However, only a minor part of the sediments transported by the Lena River enters the Laptev Sea shelf through the main channels of the delta, while the rest is dispersed within the network of the Lena Delta. Because the Lena River drains a large basin of 2.5 x lo6 km2,the chemical composition of the SPM shows a very uniform composition. -
Plumulitid Machaeridian Remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia
NORWEGIAN JOURNAL OF GEOLOGY Plumulitid mochoeridion remains from the Silurion, Arctic Russio 53 Plumulitid machaeridian remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia Anette E.S. Hogstrom, Olga K. Bogolepova & Alexander P. Gubanov Hogstrom, A.E.S., Bogolepova, O.K. and Gubanov, A.P.: Plumulitid machaeridian remains from the Silurian (Telychian) of Sevemaya Zemlya, Arc tic Russia. Norsk Geologisk Tidsskrift, Vol. 82, pp. 53-55. Trondheim 2002, ISSN 029-196X. The machaeridian genus Plumulites is reported for the first time from the Severnaya ZemlyaArchipelago of Arctic Russia, where it occurs in limes tone concretions within the Sredninskaya Formation. Graptolites fromthe same concretions indicate the late crispus- griestoniensisBiozones of the mid Telychian (Uandovery). Similarities to plumulitid sclerites from the Upper Ordovician of the Tairnyr Peninsula promotes further interest in machaeridian faunas fromthis region. A.E.S. Hogstromi, O.K. Bogolepova and A.P. Gubanov, Historical Geology & Palaeontology, Dept. of Earth Sciences, Uppsala University, Norbyviigen 22, SE-752 36, Uppsala, Sweden. I Temporaryaddress: Dept. of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol BSB l RJ, UK. lntroduction Stratigraphy and locality The global record of Silurian machaeridians is limited, Machaeridians discussed herein originate from the but includes rare articulated specimens, and more com Lower Silurian Sredninskaya Formation (Matukhin et monly isolated sclerites that have been found in Britain al. 1999). To avoid nomenclatural questions, it should (de Koninck 1857; Woodward 1865; Withers 1926 and be noted that these rocks were previously referred to as Adrain et al. 1991), the Baltic Region (Aurivillius 1892; the Golomaynnaya Formation (Menner et al. -
THE SUBSISTENCE HARVEST and USE of STELLER SEA LIONS in ALASKA by Terry L Haynes and Craig Mishler Technical Paper No
THE SUBSISTENCE HARVEST AND USE OF STELLER SEA LIONS IN ALASKA by Terry L Haynes and Craig Mishler Technical Paper No. 198 This research was partially supported by ANILCA Federal Aid funds administered through the U.S. Fish and Wildlife Service, Anchorage, Alaska, SG-1-9 Alaska Department of Fish and Game Division of Subsistence Juneau, Alaska July 1991 EEO STATEMENT The Alaska Department of Fish and Game operates all of its public programs and activities free from discrimination on the basis of race, igion, color, national origin, age, sex, or handicap Because the de partment receives federal funding, any person who believes he or she has been discriminated against should write to: O.E.O. U.S. Department of the Interior Washington, D.C. 20240 i ABSTRACT Subsequent to the classification of the Steller sea lion as a threatened species in 1990, a Sea Lion Recovery Team was created and charged with preparing a population recovery plan. This report examines the historical literature on subsistence uses, reviews Native oral traditions, and summarizes the limited amount of available information on contemporary harvests and uses of sea lions over a wide range of 25 coastal Alaskan communities. The report is designed to assist in creation of a recovery plan sensitive to subsistence uses. Further research and data needs are identified for consideration in the development of a long-range sea lion management plan. Various strategies of hunting sea lions are described, along with hunting technologies, methods of butchering sea lions, and traditional ways of cooking and serving them. Evidence gathered from prehistoric sites is summarized, and the pervasive symbolic role of Steller sea lions in Koniag and Aleut folktales, folk songs, and folk beliefs is examined in some detail. -
Hunting and Social Behaviour of Leopard Seals (Hydrurga Leptonyx) at Seal Island, South Shetland Islands, Antarctica
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Publications, Agencies and Staff of the U.S. Department of Commerce U.S. Department of Commerce 1999 Hunting and social behaviour of leopard seals (Hydrurga leptonyx) at Seal Island, South Shetland Islands, Antarctica Lisa M. Hiruki National Marine Mammal Laboratory, Alaska Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration, [email protected] Michael K. Schwartz National Marine Mammal Laboratory, Alaska Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration Peter L. Boveng National Marine Mammal Laboratory, Alaska Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration Follow this and additional works at: https://digitalcommons.unl.edu/usdeptcommercepub Part of the Environmental Sciences Commons Hiruki, Lisa M.; Schwartz, Michael K.; and Boveng, Peter L., "Hunting and social behaviour of leopard seals (Hydrurga leptonyx) at Seal Island, South Shetland Islands, Antarctica" (1999). Publications, Agencies and Staff of the U.S. Department of Commerce. 151. https://digitalcommons.unl.edu/usdeptcommercepub/151 This Article is brought to you for free and open access by the U.S. Department of Commerce at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications, Agencies and Staff of the U.S. Department of Commerce by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. J. Zool., Lond. (1999) 249, 97±109 # 1999 The Zoological Society of London Printed in the United Kingdom Hunting and social behaviour of leopard seals (Hydrurga leptonyx) at Seal Island, South Shetland Islands, Antarctica Lisa M. Hiruki*, Michael K. Schwartz{ and Peter L. -
Natural Variability of the Arctic Ocean Sea Ice During the Present Interglacial
Natural variability of the Arctic Ocean sea ice during the present interglacial Anne de Vernala,1, Claude Hillaire-Marcela, Cynthia Le Duca, Philippe Robergea, Camille Bricea, Jens Matthiessenb, Robert F. Spielhagenc, and Ruediger Steinb,d aGeotop-Université du Québec à Montréal, Montréal, QC H3C 3P8, Canada; bGeosciences/Marine Geology, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany; cOcean Circulation and Climate Dynamics Division, GEOMAR Helmholtz Centre for Ocean Research, 24148 Kiel, Germany; and dMARUM Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, 28334 Bremen, Germany Edited by Thomas M. Cronin, U.S. Geological Survey, Reston, VA, and accepted by Editorial Board Member Jean Jouzel August 26, 2020 (received for review May 6, 2020) The impact of the ongoing anthropogenic warming on the Arctic such an extrapolation. Moreover, the past 1,400 y only encom- Ocean sea ice is ascertained and closely monitored. However, its pass a small fraction of the climate variations that occurred long-term fate remains an open question as its natural variability during the Cenozoic (7, 8), even during the present interglacial, on centennial to millennial timescales is not well documented. i.e., the Holocene (9), which began ∼11,700 y ago. To assess Here, we use marine sedimentary records to reconstruct Arctic Arctic sea-ice instabilities further back in time, the analyses of sea-ice fluctuations. Cores collected along the Lomonosov Ridge sedimentary archives is required but represents a challenge (10, that extends across the Arctic Ocean from northern Greenland to 11). Suitable sedimentary sequences with a reliable chronology the Laptev Sea were radiocarbon dated and analyzed for their and biogenic content allowing oceanographical reconstructions micropaleontological and palynological contents, both bearing in- can be recovered from Arctic Ocean shelves, but they rarely formation on the past sea-ice cover. -
Dipole Anomaly in the Winter Arctic Atmosphere and Its Association with Sea Ice Motion
210 JOURNAL OF CLIMATE VOLUME 19 Dipole Anomaly in the Winter Arctic Atmosphere and Its Association with Sea Ice Motion BINGYI WU Chinese Academy of Meteorological Sciences, Beijing, China, and Institute of Marine Science, University of Alaska Fairbanks, Fairbanks, Alaska JIA WANG AND JOHN E. WALSH International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, Alaska (Manuscript submitted 5 April 2004, in final form 14 August 2005) ABSTRACT This paper identified an atmospheric circulation anomaly–dipole structure anomaly in the Arctic atmo- sphere and its relationship with winter sea ice motion, based on the International Arctic Buoy Program (IABP) dataset (1979–98) and datasets from the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) for the period 1960–2002. The dipole anomaly corresponds to the second-leading mode of EOF of monthly mean sea level pressure (SLP) north of 70°N during the winter season (October–March) and accounts for 13% of the variance. One of its two anomalous centers is stably occupied between the Kara Sea and Laptev Sea; the other is situated from the Canadian Archipelago through Greenland extending southeastward to the Nordic seas. The dipole anomaly differs from one described in other papers that can be attributed to an eastward shift of the center of action of the North Atlantic Oscillation. The finding shows that the dipole anomaly also differs from the “Barents Oscillation” revealed in a study by Skeie. Since the dipole anomaly shows a strong meridionality, it becomes an important mechanism to drive both anomalous sea ice exports out of the Arctic Basin and cold air outbreaks into the Barents Sea, the Nordic seas, and northern Europe.