Distribution of Life in the Oceans
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Methane Cold Seeps As Biological Oases in the High‐
LIMNOLOGY and Limnol. Oceanogr. 00, 2017, 00–00 VC 2017 The Authors Limnology and Oceanography published by Wiley Periodicals, Inc. OCEANOGRAPHY on behalf of Association for the Sciences of Limnology and Oceanography doi: 10.1002/lno.10732 Methane cold seeps as biological oases in the high-Arctic deep sea Emmelie K. L. A˚ strom€ ,1* Michael L. Carroll,1,2 William G. Ambrose, Jr.,1,2,3,4 Arunima Sen,1 Anna Silyakova,1 JoLynn Carroll1,2 1CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway 2Akvaplan-niva, FRAM – High North Research Centre for Climate and the Environment, Tromsø, Norway 3Division of Polar Programs, National Science Foundation, Arlington, Virginia 4Department of Biology, Bates College, Lewiston, Maine Abstract Cold seeps can support unique faunal communities via chemosynthetic interactions fueled by seabed emissions of hydrocarbons. Additionally, cold seeps can enhance habitat complexity at the deep seafloor through the accretion of methane derived authigenic carbonates (MDAC). We examined infaunal and mega- faunal community structure at high-Arctic cold seeps through analyses of benthic samples and seafloor pho- tographs from pockmarks exhibiting highly elevated methane concentrations in sediments and the water column at Vestnesa Ridge (VR), Svalbard (798 N). Infaunal biomass and abundance were five times higher, species richness was 2.5 times higher and diversity was 1.5 times higher at methane-rich Vestnesa compared to a nearby control region. Seabed photos reveal different faunal associations inside, at the edge, and outside Vestnesa pockmarks. Brittle stars were the most common megafauna occurring on the soft bottom plains out- side pockmarks. -
Bathyal Zones of the Mediterranean Continental Slope: an Attempt
Publ: Espec. but. Esp. Oceanogr. 23. 1997: 23-33 P UBUCACIONES ESPECIALES L"lSTlTUTO ESP.I\NOL DE O CEANOGRAFIA ISSN; 021-1-7378 . ISBN: 81 ~19 1 -O 299-5 Ib Ministerio de Agriculrura, Pesca yAlimentacion , L997 Bathyal zones of the Mediterranean continental slope: An attempt c. C. Emig Centre d'Ocean ologie de Marseille (UMR-CNRS 6540) , Station Mari ne d 'Endoum e, Rue de la Batterie-des-Lions. 13007 Marseille, France. Received Febru ary 1996. A ccepted August 1 99 6. ABSTRACT On the con tine ntal slop e, th e bathyal can be divided into two zones, the upper bathya l and the middle bath yal, at the shelf break, which represents th e boun dary betwe en the coastal shelf environment an d the deep realm , located at about 100-110 m dep th. T he upper bathyal, previ ously considered a transitional zone, is characterised by distin ct physical, geological an d biol ogi cal features. Its bath ymen-ic extension is directly related to slope physiography, and its lower boun dary ge ne rally corresponds to the mud line. T his belt is governe d by specific abiotic factors with stee p physical grad ients (e.g., hydro dynam ics, salin ity, oxygen , temperat ure , sedirnen ts}. Major change in tbe benthic fauna is associated with major ch ange in these abiotic factors. The three main biocoeno ses are dominated by suspen sion-feed ing species, which are exclusive to th e Mediterran ean upper bathyal. Dep ending on water parameters, the limit between th e phytal and aphyta l systems gene ra lly occurs with in th e upper bathyal. -
8.4 the Significance of Ocean Deoxygenation for Continental Margin Mesopelagic Communities J
8.4 The significance of ocean deoxygenation for continental margin mesopelagic communities J. Anthony Koslow 8.4 The significance of ocean deoxygenation for continental margin mesopelagic communities J. Anthony Koslow Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia and Scripps Institution of Oceanography, University of California, SD, La Jolla, CA 92093 USA. Email: [email protected] Summary • Global climate models predict global warming will lead to declines in midwater oxygen concentrations, with greatest impact in regions of oxygen minimum zones (OMZ) along continental margins. Time series from these regions indicate that there have been significant changes in oxygen concentration, with evidence of both decadal variability and a secular declining trend in recent decades. The areal extent and volume of hypoxic and suboxic waters have increased substantially in recent decades with significant shoaling of hypoxic boundary layers along continental margins. • The mesopelagic communities in OMZ regions are unique, with the fauna noted for their adaptations to hypoxic and suboxic environments. However, mesopelagic faunas differ considerably, such that deoxygenation and warming could lead to the increased dominance of subtropical and tropical faunas most highly adapted to OMZ conditions. • Denitrifying bacteria within the suboxic zones of the ocean’s OMZs account for about a third of the ocean’s loss of fixed nitrogen. Denitrification in the eastern tropical Pacific has varied by about a factor of 4 over the past 50 years, about half due to variation in the volume of suboxic waters in the Pacific. Continued long- term deoxygenation could lead to decreased nutrient content and hence decreased ocean productivity and decreased ocean uptake of carbon dioxide (CO2). -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The Intertidal Zone is the narrow belt along the shoreline lying between the lowest and highest tide marks. The intertidal or littoral zone is subdivided broadly into four vertical zones based on the amount of time the zone is submerged. From highest to lowest, they are Supratidal or Spray Zone Upper Intertidal submergence time Middle Intertidal Littoral Zone influenced by tides Lower Intertidal Subtidal Sublittoral Zone permanently submerged The intertidal zone may also be subdivided on the basis of the vertical distribution of the species that dominate a particular zone. However, zone divisions should, in most cases, be regarded as approximate! No single system of subdivision gives perfectly consistent results everywhere. Please refer to the intertidal zonation scheme given in the attached table (last page). Zonal Distribution of organisms is controlled by PHYSICAL factors (which set the UPPER limit of each zone): 1) tidal range 2) wave exposure or the degree of sheltering from surf 3) type of substrate, e.g., sand, cobble, rock 4) relative time exposed to air (controls overheating, desiccation, and salinity changes). BIOLOGICAL factors (which set the LOWER limit of each zone): 1) predation 2) competition for space 3) adaptation to biological or physical factors of the environment Species dominance patterns change abruptly in response to physical and/or biological factors. For example, tide pools provide permanently submerged areas in higher tidal zones; overhangs provide shaded areas of lower temperature; protected crevices provide permanently moist areas. Such subhabitats within a zone can contain quite different organisms from those typical for the zone. -
The Distributions Of, and Relationship Between, 3He and Nitrate in Eddies
ARTICLE IN PRESS Deep-Sea Research II 55 (2008) 1389– 1397 Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr2 The distributions of, and relationship between, 3He and nitrate in eddies W.J. Jenkins Ã, D.J. McGillicuddy Jr., D.E. Lott III Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA article info abstract Article history: We present and discuss the distribution of 3He and its relationship to nutrients in two eddies (cyclone Accepted 4 February 2008 C1 and anticyclone A4) with a view towards examining eddy-related mechanisms whereby nutrients Available online 9 May 2008 are transported from the upper 200–300 m into the euphotic zone of the Sargasso Sea. The different Keywords: behavior of these tracers in the euphotic zone results in changes in their distributions and relationships Biogeochemical tracers that may provide important clues as to the nature of physical and biological processes involved. Tracer techniques The cyclonic eddy (C1) is characterized by substantial 3He excesses within the euphotic zone. The 3 He distribution of this excess 3He is strongly suggestive of both past and recent ongoing deep-water Eddies injection into the euphotic zone. Crude mass balance calculations suggest that an average of Atlantic Ocean approximately 1.470.7 mol mÀ2 of nitrate has been introduced into the euphotic zone of eddy C1, Sargasso Sea consistent with the integrated apparent oxygen utilization anomaly in the aphotic zone below. The 3 He–NO3 relationship within the eddy deviates substantially from the linear thermocline trend, suggestive of incomplete drawdown of nutrients and/or substantial mixing between euphotic and aphotic zone waters. -
Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats. -
Respiration in the Mesopelagic and Bathypelagic Zones of the Oceans
CHAPTER 10 Respiration in the mesopelagic and bathypelagic zones of the oceans Javier Arístegui1, Susana Agustí2, Jack J. Middelburg3, and Carlos M. Duarte2 1 Facultad de Ciencias del Mar, Universidad de las Palmas de Gran Canaria, Spain 2 IMEDEA (CSIC–UIB), Spain 3 Netherlands Institute of Ecology, The Netherlands Outline In this chapter the mechanisms of transport and remineralization of organic matter in the dark water-column and sediments of the oceans are reviewed. We compare the different approaches to estimate respiration rates, and discuss the discrepancies obtained by the different methodologies. Finally, a respiratory carbon budget is produced for the dark ocean, which includes vertical and lateral fluxes of organic matter. In spite of the uncertainties inherent in the different approaches to estimate carbon fluxes and oxygen consumption in the dark ocean, estimates vary only by a factor of 1.5. Overall, direct measurements of respiration, as well as − indirect approaches, converge to suggest a total dark ocean respiration of 1.5–1.7 Pmol C a 1. Carbon mass − balances in the dark ocean suggest that the dark ocean receives 1.5–1.6 Pmol C a 1, similar to the estimated respiration, of which >70% is in the form of sinking particles. Almost all the organic matter (∼92%) is remineralized in the water column, the burial in sediments accounts for <1%. Mesopelagic (150–1000 m) − − respiration accounts for ∼70% of dark ocean respiration, with average integrated rates of 3–4 mol C m 2 a 1, − − 6–8 times greater than in the bathypelagic zone (∼0.5 mol C m 2 a 1). -
The C-Floor and Zones
The C-Floor and zones Table of Contents ` ❖ The ocean zones ❖ Sunlight zone and twilight zone ❖ Midnight and Abyssal zone ❖ The hadal zone ❖ The c-floor ❖ The c-floor definitions ❖ The c-floor definitions pt.2 ❖ Cites ❖ The end The ocean zones 200 meters deep 1,000 Meters deep 4,000 Meters deep 6,000 Meters deep 10,944 meters deep Sunlight zone Twilight zone ❖ The sunlight zone is 200 meters from the ocean's ❖ The twilight zone is about 1,000 meters surface deep from the ❖ Animals that live here ocean's surface sharks, sea turtles, ❖ Animals that live jellyfish and seals here are gray ❖ Photosynthesis normally whales, greenland occurs in this part of the Shark and clams ocean ❖ The twilight get only a faint amount of sunlight DID YOU KNOW Did you know That no plants live That the sunlight zone in the twilight zone could be called as the because of the euphotic and means well lit amount of sunlight in greek Midnight zone Abyssal zone ❖ The midnight zone is ❖ The abyssal zone is 4,000 meters from 6,000 meters from the the ocean's surface ocean’s surface ❖ Animals that live in ❖ Animals that live in the the midnight zone Abyssal zone are fangtooth fish, pacific are, vampire squid, viperfish and giant snipe eel and spider crabs anglerfish ❖ Supports only ❖ Animals eat only the DID YOU KNOW invertebrates and DID YOU KNOW leftovers that come That only 1 percent of light fishes That most all the way from the travels through animals are sunlight zone to the the midnight zone either small or midnight zone bioluminescent The Hadal Zone (Trench ● The Hadal Zone is 10,944 meters under the ocean ● Snails, worms, and sea cucumbers live in the hadal zone ● It is pitch black in the Hadal Zone The C-Floor The C-Floor Definitions ❖ The Continental Shelf - The flat part where people can walk. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Microbial Community and Geochemical Analyses of Trans-Trench Sediments for Understanding the Roles of Hadal Environments
The ISME Journal (2020) 14:740–756 https://doi.org/10.1038/s41396-019-0564-z ARTICLE Microbial community and geochemical analyses of trans-trench sediments for understanding the roles of hadal environments 1 2 3,4,9 2 2,10 2 Satoshi Hiraoka ● Miho Hirai ● Yohei Matsui ● Akiko Makabe ● Hiroaki Minegishi ● Miwako Tsuda ● 3 5 5,6 7 8 2 Juliarni ● Eugenio Rastelli ● Roberto Danovaro ● Cinzia Corinaldesi ● Tomo Kitahashi ● Eiji Tasumi ● 2 2 2 1 Manabu Nishizawa ● Ken Takai ● Hidetaka Nomaki ● Takuro Nunoura Received: 9 August 2019 / Revised: 20 November 2019 / Accepted: 28 November 2019 / Published online: 11 December 2019 © The Author(s) 2019. This article is published with open access Abstract Hadal trench bottom (>6000 m below sea level) sediments harbor higher microbial cell abundance compared with adjacent abyssal plain sediments. This is supported by the accumulation of sedimentary organic matter (OM), facilitated by trench topography. However, the distribution of benthic microbes in different trench systems has not been well explored yet. Here, we carried out small subunit ribosomal RNA gene tag sequencing for 92 sediment subsamples of seven abyssal and seven hadal sediment cores collected from three trench regions in the northwest Pacific Ocean: the Japan, Izu-Ogasawara, and fi 1234567890();,: 1234567890();,: Mariana Trenches. Tag-sequencing analyses showed speci c distribution patterns of several phyla associated with oxygen and nitrate. The community structure was distinct between abyssal and hadal sediments, following geographic locations and factors represented by sediment depth. Co-occurrence network revealed six potential prokaryotic consortia that covaried across regions. Our results further support that the OM cycle is driven by hadal currents and/or rapid burial shapes microbial community structures at trench bottom sites, in addition to vertical deposition from the surface ocean. -
Environmental Science
LIVING THINGS AND THE ENVIRONMENT • Ecosystem: – All the living and nonliving things that ENVIRONMENTAL SCIENCE interact in a particular area – An organism obtains food, water, shelter, and other Populations and Communities things it needs to live, grow and reproduce from its surroundings – Ecosystems may contain many different habitats Science 7 Science 7 LIVING THINGS AND THE LIVING THINGS AND THEIR ENVIRONMENT ENVIRONMENT • Habitat: • Biotic Factors: – The place and organism – The living parts of any lives and obtains all the ecosystem things it needs to survive – Example: Prairie Dogs – Example: • Hawks • Prairie Dog • Ferrets • Needs: • Badgers – Food • Eagles – Water • Grass – Shelter • Plants – Etc. Science 7 Science 7 LIVING THINGS AND THEIR LIVING THINGS AND THEIR ENVIRONMENT ENVIRONMENT • Abiotic Factors: • Abiotic Factors con’t – Water: – Sunlight: • All living things • Necessary for require water for photosynthesis survival • Your body is 65% • Organisms which water use the sun form • A watermelon is the base of the 95% water food chain • Plants need water for photosynthesis for food and oxygen production Science 7 Science 7 1 LIVING THINGS AND THEIR LIVING THINGS AND THEIR ENVIRONMENT ENVIRONMENT • Abiotic Factors Con’t • Abiotic Factors con’t – Oxygen: – Temperature: • Necessary for most • The temperature of living things an area determines • Used by animals the type of for cellular organisms which respiration can live there • Ex: Polar Bears do not live in the tropics • Ex: piranha’s don’t live in the arctic Science 7 Science