Censusing Non-Fish Nekton
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Single Particle Analysis of Particulate Pollutants in Yellowstone National Park During the Winter Snowmobile Season
SINGLE PARTICLE ANALYSIS OF PARTICULATE POLLUTANTS IN YELLOWSTONE NATIONAL PARK DURING THE WINTER SNOWMOBILE SEASON. Richard E. Peterson* and Bonnie J. Tyler** * Dept. of Chemistry and Biochemistry **Dept. of Chemical Engineering Montana State University, Bozeman, MT 59717, USA [email protected] Introduction: Particulate, or aerosol, pollution is a complex mixture of organic and inorganic compounds which includes a wide range of sizes and whose composition can vary widely depending on the time of year, geographical location, and both local and long range sources. Aerosol are important because of participation in atmospheric electricity, absorption and scattering of radiation (i.e. sunlight and thus affecting climate and visibility), their role as condensation nuclei for water vapor (and thus affecting precipitation chemistry and pH), and health effects. Particles greater than 2 micrometers in diameter (coarse) are generally formed by mechanical processes while smaller particles (fine) are formed by gas to particle conversion and accumulation/coagulation of these smallest aerosol. Because particles smaller than 2.5 micrometers (USEPA PM2.5) can become trapped deep in the lungs, it is of particular interest to identify toxic substances, such as heavy metals and polyaromatic hydrocarbons, that may be present in particles of this size range. Epidemiological studies have typically used particle size as the metric for identifying adverse health effects of particulate matter (PM), largely because data on PM size is available. Data on particle composition or other characteristics are less well known, if known at all in many cases. We are evaluating the potential for using Time of Flight Secondary Ion Mass Spectroscopy (TOF-SIMS) to study the composition of single particles from atmospheric aerosol. -
Linking Mesopelagic Prey Abundance and Distribution to the Foraging
Deep–Sea Research Part II 140 (2017) 163–170 Contents lists available at ScienceDirect Deep–Sea Research II journal homepage: www.elsevier.com/locate/dsr2 Linking mesopelagic prey abundance and distribution to the foraging MARK behavior of a deep-diving predator, the northern elephant seal ⁎ Daisuke Saijoa,1, Yoko Mitanib,1, , Takuzo Abec,2, Hiroko Sasakid, Chandra Goetsche, Daniel P. Costae, Kazushi Miyashitab a Graduate School of Environmental Science, Hokkaido University, 20-5 Bentencho, Hakodate, Hokkaido 040-0051, Japan b Field Science Center for Northern Biosphere, Hokkaido University, 20-5 Bentencho, Hakodate, Hokkaido 040-0051, Japan c School of Fisheries Science, Hokkaido University, 3-1-1 Minato cho, Hakodate, Hokkaido 041-8611, Japan d Arctic Environment Research Center, National Institute of Polar Research, 10-3, Midori-cho, Tachikawa, Tokyo 190-8518, Japan e Department of Ecology & Evolutionary Biology, University of California, Santa Cruz, CA 95060, United States ARTICLE INFO ABSTRACT Keywords: The Transition Zone in the eastern North Pacific is important foraging habitat for many marine predators. Deep-scattering layer Further, the mesopelagic depths (200–1000 m) host an abundant prey resource known as the deep scattering Transition Zone layer that supports deep diving predators, such as northern elephant seals, beaked whales, and sperm whales. fi mesopelagic sh Female northern elephant seals (Mirounga angustirostris) undertake biannual foraging migrations to this myctophid region where they feed on mesopelagic fish and squid; however, in situ measurements of prey distribution and subsurface chlorophyll abundance, as well as the subsurface oceanographic features in the mesopelagic Transition Zone are limited. While concurrently tracking female elephant seals during their post-molt migration, we conducted a ship-based oceanographic and hydroacoustic survey and used mesopelagic mid-water trawls to sample the deep scattering layer. -
Deep-Sea Life Issue 8, November 2016 Cruise News Going Deep: Deepwater Exploration of the Marianas by the Okeanos Explorer
Deep-Sea Life Issue 8, November 2016 Welcome to the eighth edition of Deep-Sea Life: an informal publication about current affairs in the world of deep-sea biology. Once again we have a wealth of contributions from our fellow colleagues to enjoy concerning their current projects, news, meetings, cruises, new publications and so on. The cruise news section is particularly well-endowed this issue which is wonderful to see, with voyages of exploration from four of our five oceans from the Arctic, spanning north east, west, mid and south Atlantic, the north-west Pacific, and the Indian Ocean. Just imagine when all those data are in OBIS via the new deep-sea node…! (see page 24 for more information on this). The photo of the issue makes me smile. Angelika Brandt from the University of Hamburg, has been at sea once more with her happy-looking team! And no wonder they look so pleased with themselves; they have collected a wonderful array of life from one of the very deepest areas of our ocean in order to figure out more about the distribution of these abyssal organisms, and the factors that may limit their distribution within this region. Read more about the mission and their goals on page 5. I always appreciate feedback regarding any aspect of the publication, so that it may be improved as we go forward. Please circulate to your colleagues and students who may have an interest in life in the deep, and have them contact me if they wish to be placed on the mailing list for this publication. -
Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun
OCEANOGRAPHY – Vol.II - Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun BIOLOGICAL OCEANOGRAPHY Legendre, Louis and Rassoulzadegan, Fereidoun Laboratoire d'Océanographie de Villefranche, France. Keywords: Algae, allochthonous nutrient, aphotic zone, autochthonous nutrient, Auxotrophs, bacteria, bacterioplankton, benthos, carbon dioxide, carnivory, chelator, chemoautotrophs, ciliates, coastal eutrophication, coccolithophores, convection, crustaceans, cyanobacteria, detritus, diatoms, dinoflagellates, disphotic zone, dissolved organic carbon (DOC), dissolved organic matter (DOM), ecosystem, eukaryotes, euphotic zone, eutrophic, excretion, exoenzymes, exudation, fecal pellet, femtoplankton, fish, fish lavae, flagellates, food web, foraminifers, fungi, harmful algal blooms (HABs), herbivorous food web, herbivory, heterotrophs, holoplankton, ichthyoplankton, irradiance, labile, large planktonic microphages, lysis, macroplankton, marine snow, megaplankton, meroplankton, mesoplankton, metazoan, metazooplankton, microbial food web, microbial loop, microheterotrophs, microplankton, mixotrophs, mollusks, multivorous food web, mutualism, mycoplankton, nanoplankton, nekton, net community production (NCP), neuston, new production, nutrient limitation, nutrient (macro-, micro-, inorganic, organic), oligotrophic, omnivory, osmotrophs, particulate organic carbon (POC), particulate organic matter (POM), pelagic, phagocytosis, phagotrophs, photoautotorphs, photosynthesis, phytoplankton, phytoplankton bloom, picoplankton, plankton, -
Abundance of Gelatinous Carnivores in the Nekton Community of the Antarctic Polar Frontal Zone in Summer 1994
MARINE ECOLOGY PROGRESS SERIES Vol. 141: 139-147, 1996 Published October 3 ' Mar Ecol Prog Ser I Abundance of gelatinous carnivores in the nekton community of the Antarctic Polar Frontal Zone in summer 1994 'Alfred-Wegener-Institut fiir Polar- und Meeresforschung. ColumbusstraBe, D-27568 Bremerhaven, Germany 'British Antarctic Survey, NERC, High Cross, Madingley Road. Cambridge CB3 OET, United Kingdom ABSTRACT The species composition, abundance, vertical distribution, biovolume and carbon content of gelatinous nekton in the Antarctic Polar Frontal Zone are described from a series of RMT25 hauls collected from a series of 200 m depth layers between 0 and 1000 m. In total. 13 species of medusa, 6 species of siphonophore, 3 species of ctenophore and 1 species of salp and nemertean were ~dentified. On average gelatinous organisms contributed 69 3% to the biovolume and 30.3% to the carbon content of the samples, although the ranges were high (0 to 98.9":) and 0 to 62 G"/;,respectively). The most important contributor to the biovolume and carbon content was the scyphomedusan Pel-iphylla peri- phylla. Some specific assoc~ationsand restricted vertlcal d~stl-ibut~ons\vcrc related to trophic interac- tions among ostracods, amphipods and cnidarians. Observations made near South Georgla showed that medusae ancl ctenophores were preyed upon by albatrosses and notothen~oidflsh respectively. The results support the premise that gelatinous organisms are a major and, at tlmes, are the main compo- nent of the oceanic macroplankton/nekton community 111 the Southern Ocean KEY WORDS: Gelatinous nekton Southern Ocean Wet biomass Carbon content. Assemblages INTRODUCTION suspension feeding pelagic tunicates (salps), become dominant (Huntley et al. -
Guidance for Using Continuous Monitors in Pm Monitoring
United States Office of Air Quality EPA-454/R-98-012 Environmental Protection Planning and Standards May 1998 Agency Research Triangle Park, NC 27711 Air GUIDANCE FOR USING CONTINUOUS MONITORS IN PM2.5 MONITORING NETWORKS GUIDANCE FOR USING CONTINUOUS MONITORS IN PM2.5 MONITORING NETWORKS May 29, 1998 PREPARED BY John G. Watson1 Judith C. Chow1 Hans Moosmüller1 Mark Green1 Neil Frank2 Marc Pitchford3 PREPARED FOR Office of Air Quality Planning and Standards U.S. Environmental Protection Agency Research Triangle Park, NC 27711 1Desert Research Institute, University and Community College System of Nevada, PO Box 60220, Reno, NV 89506 2U.S. EPA/OAQPS, Research Triangle Park, NC, 27711 3National Oceanic and Atmospheric Administration, 755 E. Flamingo, Las Vegas, NV 89119 DISCLAIMER The development of this document has been funded by the U.S. Environmental Protection Agency, under cooperative agreement CX824291-01-1, and by the Desert Research Institute of the University and Community College System of Nevada. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. This draft has not been subject to the Agency’s peer and administrative review, and does not necessarily represent Agency policy or guidance. ii ABSTRACT This guidance provides a survey of alternatives for continuous in-situ measurements of suspended particles, their chemical components, and their gaseous precursors. Recent and anticipated advances in measurement technology provide reliable and practical instruments for particle quantification over averaging times ranging from minutes to hours. These devices provide instantaneous, telemetered results and can use limited manpower more efficiently than manual, filter-based methods. -
Arctic Marine Biodiversity
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/292115665 Arctic marine biodiversity CHAPTER · JANUARY 2016 READS 142 12 AUTHORS, INCLUDING: Lis Lindal Jørgensen Philippe Archambault Institute of Marine Research in Norway Université du Québec à Rimouski UQAR 36 PUBLICATIONS 285 CITATIONS 137 PUBLICATIONS 1,574 CITATIONS SEE PROFILE SEE PROFILE Dieter Piepenburg Jake Rice Christian-Albrechts-Universität zu Kiel Fisheries and Oceans Canada 71 PUBLICATIONS 1,705 CITATIONS 67 PUBLICATIONS 2,279 CITATIONS SEE PROFILE SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: Andrey V. Dolgov letting you access and read them immediately. Retrieved on: 19 February 2016 Chapter 36G. Arctic Ocean Contributors: Lis Lindal Jørgensen, Philippe Archambault, Claire Armstrong, Andrey Dolgov, Evan Edinger, Tony Gaston, Jon Hildebrand, Dieter Piepenburg, Walker Smith, Cecilie von Quillfeldt, Michael Vecchione, Jake Rice (Lead member) Referees: Arne Bjørge, Charles Hannah. 1. Introduction 1.1 State The Central Arctic Ocean and the marginal seas such as the Chukchi, East Siberian, Laptev, Kara, White, Greenland, Beaufort, and Bering Seas, Baffin Bay and the Canadian Archipelago (Figure 1) are among the least-known basins and bodies of water in the world ocean, because of their remoteness, hostile weather, and the multi-year (i.e., perennial) or seasonal ice cover. Even the well-studied Barents and Norwegian Seas are partly ice covered during winter and information during this period is sparse or lacking. The Arctic has warmed at twice the global rate, with sea- ice loss accelerating (Figure 2, ACIA, 2004; Stroeve et al., 2012, Chapter 46 in this report), especially along the coasts of Russia, Alaska, and the Canadian Archipelago (Post et al., 2013). -
Chapter 12 Lecture
ChapterChapter 1 12 Clickers Lecture Essentials of Oceanography Eleventh Edition Marine Life and the Marine Environment Alan P. Trujillo Harold V. Thurman © 2014 Pearson Education, Inc. Chapter Overview • Living organisms, including marine species, are classified by characteristics. • Marine organisms are adapted to the ocean’s physical properties. • The marine environment has distinct divisions. © 2014 Pearson Education, Inc. Classification of Life • Classification based on physical characteristics • DNA sequencing allows genetic comparison. © 2014 Pearson Education, Inc. Classification of Life • Living and nonliving things made of atoms • Life consumes energy from environment. • NASA’s definition encompasses potential for extraterrestrial life. © 2014 Pearson Education, Inc. Classification of Life • Working definition of life • Living things can – Capture, store, and transmit energy – Reproduce – Adapt to environment – Change over time © 2014 Pearson Education, Inc. Classification of Life • Three domains or superkingdoms • Bacteria – simple life forms without nuclei • Archaea – simple, microscopic creatures • Eukarya – complex, multicellular organisms – Plants and animals – DNA in discrete nucleus © 2014 Pearson Education, Inc. Classification of Living Organisms • Five kingdoms – Monera – Protoctista – Fungi – Plantae – Animalia © 2014 Pearson Education, Inc. Five Kingdoms of Organisms • Monera – Simplest organisms, single-celled – Cyanobacteria, heterotrophic bacteria, archaea • Protoctista – Single- and multicelled with nucleus – -
Meridional Patterns in the Deep Scattering Layers and Top Predator Distribution in the Central Equatorial Pacific
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 2010 Meridional patterns in the deep scattering layers and top predator distribution in the central equatorial Pacific Elliott L. Hazen NOAA SWFSC Pacific Fisheries Environmental Lab, [email protected] David W. Johnston Duke University Marine Lab, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/usdeptcommercepub Part of the Environmental Sciences Commons Hazen, Elliott L. and Johnston, David W., "Meridional patterns in the deep scattering layers and top predator distribution in the central equatorial Pacific" (2010). Publications, Agencies and Staff of the U.S. Department of Commerce. 275. https://digitalcommons.unl.edu/usdeptcommercepub/275 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. FISHERIES OCEANOGRAPHY Fish. Oceanogr. 19:6, 427–433, 2010 SHORT COMMUNICATION Meridional patterns in the deep scattering layers and top predator distribution in the central equatorial Pacific ELLIOTT L. HAZEN1,2,* AND DAVID W. component towards understanding the behavior and JOHNSTON1 distribution of highly migratory predator species. 1 Division of Marine -
Chapter 15 Marrone
Chapter 15 Life Near the Surface Pelagic Zone • Pelagic Zone – The vast open sea – Contains almost all of the liquid water on earth Pelagic Zone • Pelagic zone benefits – Regulates our climate – Provides food. • Pelagic organisms live suspended in the water • Lacks the solid substrate provided by the bottom • No place for attachment, no bottom for burrowing, nothing to hide behind Epipelagic Zone • Epipelagic – Upper pelagic – Zone from the surface down to a given depth commonly 200 m (650 ft) – Warmest – Best lit • The photic zone - area where photosynthesis can occur Epipelagic Zone • The epipelagic zone has two main components • Coastal or Nertic – epipelagic waters that lie over the continental shelf – Lies close to shore – Supports most of the world’s marine fisheries production • Oceanic part – Waters beyond the continental shelf The Organisms of the Epipelagic The Epipelagic Zone • Fueled by solar energy captured in photosynthesis • Nearly all primary production takes place within the epiplagic zone. • Supplies food to other communities The Epipelagic Zone • Lacks deposit feeders • Suspension feeders are very common • There are also many large predators like fishes, squids and marine mammals • Plankton is abundant Plankton Plankton • Plankton - live in the water column and cannot swim against the current. • Phytoplankton are autotrophs. – Perform photosynthesis • Zooplankton – are heterotrophs • Plankton can be grouped based on their size – Picoplankton – smallest – Nanoplankton – Microplankton – Mesoplankton – Macroplankton – -
Deep-Sea Life Issue 14, January 2020 Cruise News E/V Nautilus Telepresence Exploration of the U.S
Deep-Sea Life Issue 14, January 2020 Welcome to the 14th edition of Deep-Sea Life (a little later than anticipated… such is life). As always there is bound to be something in here for everyone. Illustrated by stunning photography throughout, learn about the deep-water canyons of Lebanon, remote Pacific Island seamounts, deep coral habitats of the Caribbean Sea, Gulf of Mexico, Southeast USA and the North Atlantic (with good, bad and ugly news), first trials of BioCam 3D imaging technology (very clever stuff), new deep pelagic and benthic discoveries from the Bahamas, high-risk explorations under ice in the Arctic (with a spot of astrobiology thrown in), deep-sea fauna sensitivity assessments happening in the UK and a new photo ID guide for mesopelagic fish. Read about new projects to study unexplored areas of the Mid-Atlantic Ridge and Azores Plateau, plans to develop a water-column exploration programme, and assessment of effects of ice shelf collapse on faunal assemblages in the Antarctic. You may also be interested in ongoing projects to address and respond to governance issues and marine conservation. It’s all here folks! There are also reports from past meetings and workshops related to deep seabed mining, deep-water corals, deep-water sharks and rays and information about upcoming events in 2020. Glance over the many interesting new papers for 2019 you may have missed, the scientist profiles, job and publishing opportunities and the wanted section – please help your colleagues if you can. There are brief updates from the Deep- Ocean Stewardship Initiative and for the deep-sea ecologists amongst you, do browse the Deep-Sea Biology Society president’s letter. -
Glossary Animal Physiology
Limnology 1 Weisse - WS99/00 Glossary Limnology 1 Biological Zonation of a lentic System: Most organisms can be classified on the basis of their typical habitat. Benthos: The community of plants and animals that live permanently in or on the sea bottom. Littoral (intertidal zone): The trophogenic zone along the shore till the compensation depth where NPP occurs. It is rich in species diversity and number - especially algae and higher plants. • Epilittoral: Sedentary organisms of the shoreline; e.g. macrophytes, diatoms, etc. • Profundal: Depths of 180m and deeper. Limnion: Temperature related zonation of the open water body of lentic systems; i.e. summer stratification due to solar radiation produces several trophic zones - see also ecological aspects - depth zones. • Epilimnion: The upper warm and illuminated surface layer of a lake; narrower than the trophogenic zone. • Metalimnion: The transitional zone between epi- and hypolimnion; i.e. the zone of the thermocline. • Hypolimnion: The cool and poorly illuminated bottom layer of a lake, below the thermocline. Nekton: Pelagic animals that are active swimmers; i.e. most of the adult fishes. Pelagial: The environment of the open water of a lake, away from the bottom, and not in close proximity to the shoreline. It is Lower in species number and diversity than the benthos. The pelagial of rivers exhibits a directed and continuos flux (spatial relocation = amountH2O/cross-surface area). Plankton: Passively drifting or weakly swimming organisms in fresh waters; i.e. microscopic plants, eggs, larval stages of the nekton and benthos (such as phyto-plankton, zoo-plankton). • Neuston: The epipelagic zone few centimeters below the waterline; i.e.