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Marine Ecology Progress Series 600:21
Vol. 600: 21–39, 2018 MARINE ECOLOGY PROGRESS SERIES Published July 30 https://doi.org/10.3354/meps12663 Mar Ecol Prog Ser OPENPEN ACCESSCCESS Short-term processing of ice algal- and phytoplankton- derived carbon by Arctic benthic communities revealed through isotope labelling experiments Anni Mäkelä1,*, Ursula Witte1, Philippe Archambault2 1School of Biological Sciences, University of Aberdeen, Aberdeen AB24 3UU, UK 2Département de biologie, Québec Océan, Université Laval, Québec, QC G1V 0A6, Canada ABSTRACT: Benthic ecosystems play a significant role in the carbon (C) cycle through remineral- ization of organic matter reaching the seafloor. Ice algae and phytoplankton are major C sources for Arctic benthic consumers, but climate change-mediated loss of summer sea ice is predicted to change Arctic marine primary production by increasing phytoplankton and reducing ice algal contributions. To investigate the impact of changing algal C sources on benthic C processing, 2 isotope tracing experiments on 13C-labelled ice algae and phytoplankton were conducted in the North Water Polynya (NOW; 709 m depth) and Lancaster Sound (LS; 794 m) in the Canadian Arc- tic, during which the fate of ice algal (CIA) and phytoplankton (CPP) C added to sediment cores was traced over 4 d. No difference in sediment community oxygen consumption (SCOC, indicative of total C turnover) between the background measurements and ice algal or phytoplankton cores was found at either site. Most of the processed algal C was respired, with significantly more CPP than CIA being released as dissolved inorganic C at both sites. Macroinfaunal uptake of algal C was minor, but bacterial assimilation accounted for 33−44% of total algal C processing, with no differences in bacterial uptake of CPP and CIA found at either site. -
Phytoplankton As Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate
sustainability Review Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate Samarpita Basu * ID and Katherine R. M. Mackey Earth System Science, University of California Irvine, Irvine, CA 92697, USA; [email protected] * Correspondence: [email protected] Received: 7 January 2018; Accepted: 12 March 2018; Published: 19 March 2018 Abstract: The world’s oceans are a major sink for atmospheric carbon dioxide (CO2). The biological carbon pump plays a vital role in the net transfer of CO2 from the atmosphere to the oceans and then to the sediments, subsequently maintaining atmospheric CO2 at significantly lower levels than would be the case if it did not exist. The efficiency of the biological pump is a function of phytoplankton physiology and community structure, which are in turn governed by the physical and chemical conditions of the ocean. However, only a few studies have focused on the importance of phytoplankton community structure to the biological pump. Because global change is expected to influence carbon and nutrient availability, temperature and light (via stratification), an improved understanding of how phytoplankton community size structure will respond in the future is required to gain insight into the biological pump and the ability of the ocean to act as a long-term sink for atmospheric CO2. This review article aims to explore the potential impacts of predicted changes in global temperature and the carbonate system on phytoplankton cell size, species and elemental composition, so as to shed light on the ability of the biological pump to sequester carbon in the future ocean. -
Deep-Sea Mining: the Basics
A fact sheet from June 2018 NOAA Office of Ocean Exploration and Research Deep-sea Mining: The Basics Overview The deepest parts of the world’s ocean feature ecosystems found nowhere else on Earth. They provide habitat for multitudes of species, many yet to be named. These vast, lightless regions also possess deposits of valuable minerals in rich concentrations. Deep-sea extraction technologies may soon develop to the point where exploration of seabed minerals can give way to active exploitation. The International Seabed Authority (ISA) is charged with formulating and enforcing rules for all seabed mining that takes place in waters beyond national jurisdictions. These rules are now under development. Environmental regulations, liability and financial rules, and oversight and enforcement protocols all must be written and approved within three to five years. Figure 1 Types of Deep-sea Mining Production support vessel Return pipe Riser pipe Cobalt Seafloor massive Polymetallic crusts sulfides nodules Subsurface plumes 800-2,500 from return water meters deep Deposition 1,000-4,000 meters deep 4,000-6,500 meters deep Cobalt-rich Localized plumes Seabed pump Ferromanganeseferromanganese from cutting crusts Seafloor production tool Nodule deposit Massive sulfide deposit Sediment Source: New Zealand Environment Guide © 2018 The Pew Charitable Trusts 2 The legal foundations • The United Nations Convention on the Law of the Sea (UNCLOS). Also known as the Law of the Sea Treaty, UNCLOS is the constitutional document governing mineral exploitation on the roughly 60 percent of the world seabed that lies beyond national jurisdictions. UNCLOS took effect in 1994 upon passage of key enabling amendments designed to spur commercial mining. -
Seabed Mapping: a Brief History from Meaningful Words
geosciences Review Seabed Mapping: A Brief History from Meaningful Words Pedro Smith Menandro and Alex Cardoso Bastos * Marine Geosciences Lab (Labogeo), Departmento Oceanografia, Universidade Federal do Espírito Santo, Vitória-ES 29075-910, Brazil; [email protected] * Correspondence: [email protected] Received: 19 May 2020; Accepted: 7 July 2020; Published: 16 July 2020 Abstract: Over the last few centuries, mapping the ocean seabed has been a major challenge for marine geoscientists. Knowledge of seabed bathymetry and morphology has significantly impacted our understanding of our planet dynamics. The history and scientific trends of seabed mapping can be assessed by data mining prior studies. Here, we have mined the scientific literature using the keyword “seabed mapping” to investigate and provide the evolution of mapping methods and emphasize the main trends and challenges over the last 90 years. An increase in related scientific production was observed in the beginning of the 1970s, together with an increased interest in new mapping technologies. The last two decades have revealed major shift in ocean mapping. Besides the range of applications for seabed mapping, terms like habitat mapping and concepts of seabed classification and backscatter began to appear. This follows the trend of investments in research, science, and technology but is mainly related to national and international demands regarding defining that country’s exclusive economic zone, the interest in marine mineral and renewable energy resources, the need for spatial planning, and the scientific challenge of understanding climate variability. The future of seabed mapping brings high expectations, considering that this is one of the main research and development themes for the United Nations Decade of the Oceans. -
Drivers and Effects of Karenia Mikimotoi Blooms in the Western English Channel ⇑ Morvan K
Progress in Oceanography 137 (2015) 456–469 Contents lists available at ScienceDirect Progress in Oceanography journal homepage: www.elsevier.com/locate/pocean Drivers and effects of Karenia mikimotoi blooms in the western English Channel ⇑ Morvan K. Barnes a,1, Gavin H. Tilstone a, , Timothy J. Smyth a, Claire E. Widdicombe a, Johanna Gloël a,b, Carol Robinson b, Jan Kaiser b, David J. Suggett c a Plymouth Marine Laboratory, Prospect Place, West Hoe, Plymouth PL1 3DH, UK b Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK c Functional Plant Biology & Climate Change Cluster, University of Technology Sydney, PO Box 123, Broadway, NSW 2007, Australia article info abstract Article history: Naturally occurring red tides and harmful algal blooms (HABs) are of increasing importance in the coastal Available online 9 May 2015 environment and can have dramatic effects on coastal benthic and epipelagic communities worldwide. Such blooms are often unpredictable, irregular or of short duration, and thus determining the underlying driving factors is problematic. The dinoflagellate Karenia mikimotoi is an HAB, commonly found in the western English Channel and thought to be responsible for occasional mass finfish and benthic mortali- ties. We analysed a 19-year coastal time series of phytoplankton biomass to examine the seasonality and interannual variability of K. mikimotoi in the western English Channel and determine both the primary environmental drivers of these blooms as well as the effects on phytoplankton productivity and oxygen conditions. We observed high variability in timing and magnitude of K. mikimotoi blooms, with abun- dances reaching >1000 cells mLÀ1 at 10 m depth, inducing up to a 12-fold increase in the phytoplankton carbon content of the water column. -
Worksheets on Climate Change: Sea Level Rise
EDUCATION FOR SUSTAINABLE DEVELOPMENT WORKSHEETS ON CLIMATE CHANGE Sea level rise Consequences for coastal and lowland areas: Bangladesh and the Netherlands Sea level rise – Consequences for coastal and lowland areas: Bangladesh and the Netherlands © Germanwatch 2014 Sea level rise Consequences for coastal and lowland areas: Bangladesh and the Netherlands As a consequence of the anthropogenic greenhouse effect A comparison of the two countries, the Netherlands and the scientific community predicts an increase in average Bangladesh, both of which are potentially very much jeop- global temperature and resulting sea level rise. Heated ardised by sea level rise, clearly illustrates the likely im- water, however, expands only slowly because of the heat pacts for humans and the environment, but also shows transfer from the atmosphere to the sea. For this reason, how different the capacities of individual countries are the sea responds to climate change like a slow-to-react concerning their ability to adapt and to protect them- monster – slow but persistent. In the 20th century the selves from the consequences. Bangladesh, one of the sea level already rose by an average of 12 to 22 cm. The poorest and at the same time most densely populated Intergovernmental Panel on Climate Change (IPCC) con- countries in the world, is also one of the countries which cludes that, as a result of climate change, by 2100 the rise will be most affected by the expected sea level rise. in sea levels could increase worldwide by up to almost 1 metre compared to the mean sea level in the years Flooding has already caused damage up to 100 km inland 1986–2005. -
Modelling an Alkenone-Like Proxy Record in the NW African Upwelling
Biogeosciences, 3, 251–269, 2006 www.biogeosciences.net/3/251/2006/ Biogeosciences © Author(s) 2006. This work is licensed under a Creative Commons License. Modelling an alkenone-like proxy record in the NW African upwelling X. Giraud Research Center Ocean Margins, Universitat¨ Bremen, Postfach 330 440, 28 334 Bremen, Germany Received: 28 November 2005 – Published in Biogeosciences Discuss.: 27 January 2006 Revised: 16 May 2006 – Accepted: 30 May 2006 – Published: 21 June 2006 Abstract. A regional biogeochemical model is applied to temperature of these algae (Marlowe, 1984; Brassell et al., the NW African coastal upwelling between 19◦ N and 27◦ N 1986; Conte et al., 1998). Prahl et al. (1988) calibrated a lin- K0 to investigate how a water temperature proxy, alkenones, are ear relation between an unsaturation alkenone index (U37 ) produced at the sea surface and recorded in the slope sed- and the growth temperature of an E. huxleyi strain in cul- iments. The biogeochemical model has two phytoplankton ture experiments. It was then confirmed that this index could groups: an alkenone producer group, considered to be coc- be used in the open ocean to reconstruct SSTs from coretop colithophores, and a group comprising other phytoplankton. alkenone measurements (Muller¨ et al., 1998). K0 The Regional Ocean Modelling System (ROMS) is used to In order to be used as a paleotemperature proxy, the U37 simulate the ocean circulation and takes advantage of the K0 has to fulfil certain criteria. The stability of the U37 signal Adaptive Grid Refinement in Fortran (AGRIF) package to in the water and sedimentary diagenesis are still questions. -
Pressure 4117, Tide 5217, Wave and Tide 5218
TD 302 OPERATING MANUAL PRESSURE SENSOR 4117/4117R TIDE SENSOR 5217/5217R WAVE & TIDE SENSOR 5217/5217R January 2014 PRESSURE SENSOR 4117/4117R TIDE SENSOR 5217/5217R WAVE AND TIDE SENSOR 5218/5218R Page 2 Aanderaa Data Instruments AS – TD302 1st Edition 30 June 2013 Preliminary 2nd Edition 05 September 2003 New version including general updates in text. Rebranded, Frame Work 3 update, please refer Product change notification AADI Document ID:DA-50009-01, Date: 09 December 2011 (ref Appendix 6 ). 3rd Edition 14 January 2014 New property “Installation Depth” added for Tide sensors, effective version 8.1.1 © Copyright: Aanderaa Data Instruments AS January 2014 - TD 302 Operating Manual for Pressure 4117/4117R Tide 5217/5217R, Wave & Tide 5218/5218R Page 3 Table of Contents Introduction .............................................................................................................................................................. 6 Purpose and scope ................................................................................................................................................ 6 Document overview.............................................................................................................................................. 6 Applicable documents .......................................................................................................................................... 7 Abbreviations ....................................................................................................................................................... -
Global Open Oceans and Deep Seabed (Goods) - Biogeographic Classification
CBD Distr. GENERAL UNEP/CBD/SBSTTA/14/INF/10 29 April 2010 ORIGINAL: ENGLISH SUBSIDIARY BODY ON SCIENTIFIC, TECHNICAL AND TECHNOLOGICAL ADVICE Fourteenth meeting Nairobi, 10-21 May 2010 Item 3.1.3 of the provisional agenda * GLOBAL OPEN OCEANS AND DEEP SEABED (GOODS) - BIOGEOGRAPHIC CLASSIFICATION Note by the Executive Secretary 1. The Executive Secretary is circulating herewith, for the information of participants in the fourteenth meeting of the Subsidiary Body on Scientific, Technical and Technological Advice, IOC Technical Series No.84 on Global Open Oceans and Deep Seabed (GOODS) - Biogeographic Classification, submitted by the United Nations Educational, Scientific and Cultural Organization/Intergovernmental Oceanographic Commission, pursuant to paragraph 6of decision IX/20. 2. This report was also considered by the CBD Expert Workshop on Scientific and Technical Guidance on the Use of Biogeographic Classification Systems and Identification of Marine Areas Beyond National Jurisdiction in Need of Protection, held in Ottawa, from 29 September to 2 October 2009. 3. The document is circulated in the form and language in which it was received by the Secretariat of the Convention on Biological Diversity. * UNEP/CBD/SBSTTA/14/1 /... In order to minimize the environmental impacts of the Secretariat’s processes, and to contribute to the Secretary-General’s initiative f or a C-Neutral UN, this document is printed in limited numbers. Delegates are kindly requested to bring their copies to meetings and not to request additional copies. Global Open Oceans and Deep Seabed (GOODS) biogeographic classification Global Open Oceans and Deep Seabed (GOODS) biogeographic classification Edited by: Marjo Vierros (UNU-IAS), Ian Cresswell (Australia), Elva Escobar Briones (Mexico), Jake Rice (Canada), and Jeff Ardron (Germany) UNESCO 2009 goods inside 2.indd 1 24/03/09 14:55:52 Global Open Oceans and Deep Seabed (GOODS) biogeographic classification Authors Contributors Vera N. -
Diatom Fluxes to the Deep Sea in the Oligotrophic North Pacific Gyre at Station ALOHA
MARINE ECOLOGY PROGRESS SERIES Published June 11 Mar Ecol Prog Ser Diatom fluxes to the deep sea in the oligotrophic North Pacific gyre at Station ALOHA Renate Scharek*, Luis M. Tupas, David M. Karl Department of Oceanography, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii 96822, USA ABSTRACT: Planktonic diatoms are important agents of vertical transport of photosynthetically fixed organic carbon to the ocean's interior and seafloor. Diatom fluxes to the deep sea were studied for 2 yr using bottom-moored sequencing sediment traps located in the vicinity of the Hawaii Ocean Time- series (HOT) program station 'ALOHA' (22'45'N, 158" W). The average flux of empty diatom frustules was around 2.8 X 10' cells m-' d ' in both years, except in late summer when it increased approximately 30-fold. Flux of cytoplasm-containing diatom cells was much lower (about 8 X 103 cells n1Y2 d") but increased 500-fold in late July 1992 and 1250-fold in August 1994. Mastogloia woodiana Taylor, Hemj- aulus hauckii Grunow and Rliizosolenia cf. clevei var. communis Sundstrom were the domlnant diatom species observed during the July 1992 event, with the former 2 species again dominant in August 1994. The 1994 summer flux event occurred about 3 wk after a documented bloom of H. hauckii and M. woodiana in the mixed-layer and a simultaneous increase in vertical flux of these species. This surface flux signal was clearly detectable at 4000 m, suggesting rapid settling rates. A further indication of very high sinking speeds of the diatoms was the much larger proportion of cytoplasm-containing cells in the bottom-moored traps during the 2 summer events. -
Influence of Seasonally Deposited Phytodetritus on Benthic Foraminiferal Populations in the Bathyal Northeast Atlantic: the Species Response
Vol. 58: 53-67, 1989 MARINE ECOLOGY PROGRESS SERIES Published December 15 Mar. Ecol. Prog. Ser. Influence of seasonally deposited phytodetritus on benthic foraminiferal populations in the bathyal northeast Atlantic: the species response ' Institute of Oceanographic Sciences, Deacon Laboratory. Wormley, Godalming, Surrey GU8 5UB. United Kingdom Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD. United Kingdom ABSTRACT: Cores were obtained with a multiple corer at a bathyal site (1320 to 1360m depth) in the Porcupine Seabight during April and July 1982. In July (but not April) the sediment surface was overlain by a layer of phytodetritus, material rapidly sedlmented from the euphotik zone following the spring bloom. The phytodetrital fraction of samples (0 to 1 cm layer of subcores; 3.46 cm2 surface area) removed from the July cores harboured dense, low-diversity populations of benthic foraminifers which resembled the phytodetritus-dwelling assemblages already described from the much deeper (4550 m) BIOTRANS site in the northeast Atlantic. Our new observations consolidate the view that phytodetritus is a microhabitat for some deep-sea benthic foraminiferal species. The bathyal populations were dominated by Alabaminella weddellensis (75 '70 of total) and also included Episton~inellaexigua and Tinogullmia sp. nov. These 3 species occurred also in the BIOTRANS phytodetrital assemblages. The April san~ples and the total July samples (phytodetritus plus sediment fractions) yielded diverse foraminiferal popula- tions of similar density and species richness. However, there were some important taxonomic dffer- ences. In particular, the 8 species consistently present in the phytodetritus were significantly more abundant in the July san~ples,while the most common species in the April sanlples (01.dmrnina sp. -
Coastal Marine Institute Epibenthic Community Variability on The
University of Alaska Coastal Marine Institute Epibenthic Community Variability on the Alaskan Beaufort Sea Continental Shelf Principal Investigator: Brenda Konar, University of Alaska Fairbanks Collaborator: Alexandra M. Ravelo, University of Alaska Fairbanks Final Report May 201 3 OCS Study BOEM 2013-01148 Contact Information: email: [email protected] phone: 907.474.6782 fax: 907.474.7204 Coastal Marine Institute School of Fisheries and Ocean Sciences University of Alaska Fairbanks P. O. Box 757220 Fairbanks, AK 99775-7220 This study was funded in part by the U.S. Department of the Interior, Bureau of Ocean Energy Management (BOEM) through Cooperative Agreement M11AC00002 between BOEM, Alaska Outer Continental Shelf Region, and the University of Alaska Fairbanks. This report, OCS Study BOEM 2013-01148, is available through the Coastal Marine Institute, select federal depository libraries and http://www.boem.gov/Environmental-Stewardship/Environmental-Studies/Alaska-Region/Index.aspx. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the U.S. Government. Mention of trade names or commercial products does not constitute their endorsement by the U.S. Government. Contents Figures ............................................................................................................................................. iii Tables .............................................................................................................................................