Antarctic Krill Euphausia Superba: Spatial Distribution, Abundance, and Management of Fisheries in a Changing Climate
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
An Observation of Two Oceanic Salp Swarms in the Tasman Sea: Thetys Vagina and Cyclosalpa Affinis Natasha Henschke1,2,3*, Jason D
Henschke et al. Marine Biodiversity Records (2016) 9:21 DOI 10.1186/s41200-016-0023-8 MARINE RECORD Open Access An observation of two oceanic salp swarms in the Tasman Sea: Thetys vagina and Cyclosalpa affinis Natasha Henschke1,2,3*, Jason D. Everett1,2,3 and Iain M. Suthers1,2,3 Abstract Background: Large oceanic salps are rarely encountered. The highest recorded biomasses of the salps Thetys vagina (852 g WW m−3)andCyclosalpa affinis (1149 g WW m−3) were observed in the Tasman Sea during January 2009. Results: Due to their fast sinking rates the carcasses and faecal pellets of these and other large salps play a significant role in carbon transport to the seafloor. We calculated that faecal pellets from these swarms could have contributed up to 67 % of the mean organic daily carbon flux in the area. This suggests that the flux of carbon from salp swarms are not accurately captured in current estimates. Conclusion: This study contributes information on salp abundance and biomass to a relatively understudied field, improving estimates for biogeochemical cycles. Background (Henschke et al., 2013) can increase the carbon flux in an The role of gelatinous zooplankton, such as salps, pyro- area up to ten-fold the daily average (Fischer et al., 1988) somes and cnidarians, in ocean food webs and biogeo- for a sustained period of time (Smith et al. 2014). chemical cycling has garnered increased attention in Due to their regular occurrence (Henschke et al., recent years (Lebrato et al., 2011; Henschke et al., 2013; 2014) and coastal dominance (Henschke et al 2011), Lebrato et al., 2013; Smith et al. -
Advances in Polar Ecology Series Ed.: D
Advances in Polar Ecology Series Ed.: D. Piepenburg In recent years, the polar regions have received increased scientific and public interest. Both the Arctic and Antarctic have been recognized as key regions in the regulation of the global climate and polar ecosystems have been identified to be particularly susceptible to the ongoing environmental changes. Consequently, the international efforts in polar research have been enhanced considerably, and a wealth of new findings is being produced at a growing rate by the international community of polar researchers. The aim of the book series Advances in Polar Ecology is to foster the progress in the scientific knowledge about the polar and sub-polar regions of both hemispheres by contributing to the fast and wide-ranging dissemination of novel scientific information gained from recent studies of sea, freshwater and land biota among polar researchers, environmental managers and policy makers. Advances in Polar Ecology’s broad ecology- oriented scope encompasses environmental and biological research of both recent and past ecosystems. The Series offers an outlet to publish contributions (monographs, edited works, conference proceedings, etc.) addressing scientific topics that need more comprehensive and in-depth analysis than the length of typical journal articles allow for. These include, but are not limited to, thorough accounts of the current status of active research areas of wide importance that outline promising perspectives for future research. An international editorial board oversees the rigorous peer review that all contributions will be subjected to. Springer books available as Recently published: Printed book Available from springer.com/shop J. Berge, G. Johnsen, J. -
Modelling Growth of Northern Krill (Meganyctiphanes Norvegica) Using an Energy-Budget Approach?
Modelling growth of northern krill (Meganyctiphanes norvegica) using an energy-budget approach? Tjalling Jagera,, Elisa Ravagnanb aDEBtox Research, De Bilt, the Netherlands bIRIS Environment, International Research Institute of Stavanger, Postboks 8046, N-4068 Stavanger, Norway Abstract Northern krill (Meganyctiphanes norvegica) is an important species in the North Atlantic and the Mediterranean Sea, but very little life-history infor- mation is available under controlled (laboratory) conditions. Here, we use the DEBkiss model to piece together the available data into a quantitative energy budget. We use this model to analyse larval growth curves, and to re- construct the feeding history for field populations from their (reconstructed) multi-year growth patterns. The resulting model parameters are also used to provide estimates for respiration, feeding and reproduction rates that are consistent with measured values. Many uncertainties remain, but this anal- ysis demonstrates how simple and generic energy-budget models have the potential to integrate observations on different traits, to interpret growth as a function of food and temperature, and to compare different species in a meaningful manner. Keywords: Dynamic Energy Budget, DEBkiss, Meganyctiphanes norvegica, life-history traits, growth modeling, krill ?©2016. This manuscript version is made available under the CC-BY-NC-ND 4.0 license https://creativecommons.org/licenses/by-nc-nd/4.0/. The paper was pub- lished as: Jager T, Ravagnan E. 2016. Modelling growth of northern krill (Meganyc- tiphanes norvegica) using an energy-budget approach. Ecological Modelling 325:28-34.. http://dx.doi.org/10.1016/j.ecolmodel.2015.12.020. Email address: [email protected] (Tjalling Jager) URL: http://www.debtox.nl/ (Tjalling Jager) Preprint submitted to Ecological Modelling March 14, 2021 1. -
Mitigation of Arctic Tundra Surface Warming by Plant Evapotranspiration: Complete Energy Balance Component Estimation Using LANDSAT Satellite Data
remote sensing Article Mitigation of Arctic Tundra Surface Warming by Plant Evapotranspiration: Complete Energy Balance Component Estimation Using LANDSAT Satellite Data Václav Nedbal 1,* , Kamil Láska 2,3 and Jakub Brom 1 1 Faculty of Agriculture, University of South Bohemia in Ceskˇ é Budˇejovice,Studentská 1668, 370 05 Ceskˇ é Budˇejovice,Czech Republic; [email protected] 2 Department of Geography, Faculty of Science, Masaryk University, Kotláˇrská 2, 611 37 Brno, Czech Republic; [email protected] 3 Centre for Polar Ecology, Faculty of Science, University of South Bohemia in Ceskˇ é Budˇejovice,Na Zlaté stoce 3, 370 05 Ceskˇ é Budˇejovice,Czech Republic * Correspondence: [email protected] Received: 19 September 2020; Accepted: 14 October 2020; Published: 16 October 2020 Abstract: Global climate change is expected to cause a strong temperature increase in the polar regions, accompanied by a reduction in snow cover. Due to a lower albedo, bare ground absorbs more solar energy and its temperature can increase more. Here, we show that vegetation growth in such bare ground areas can efficiently mitigate surface warming in the Arctic, thanks to plant evapotranspiration. In order to establish a comprehensive energy balance for the Arctic land surface, we used an ensemble of methods of ground-based measurements and multispectral satellite image analysis. Our estimate is that the low vegetation of polar tundra transforms 26% more solar energy into evapotranspiration than bare ground in clear sky weather. Due to its isolation properties, vegetation further reduces ground heat flux under the surface by ~4%, compared to bare areas, thus lowering the increase in subsurface temperature. -
Salp Contributions to Vertical Carbon Flux in the Sargasso Sea
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by College of William & Mary: W&M Publish W&M ScholarWorks VIMS Articles Virginia Institute of Marine Science 2016 Salp contributions to vertical carbon flux in the Sargasso Sea JP Stone Virginia Institute of Marine Science Deborah K. Steinberg Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/vimsarticles Part of the Aquaculture and Fisheries Commons Recommended Citation Stone, JP and Steinberg, Deborah K., "Salp contributions to vertical carbon flux in the Sargasso Sea" (2016). VIMS Articles. 797. https://scholarworks.wm.edu/vimsarticles/797 This Article is brought to you for free and open access by the Virginia Institute of Marine Science at W&M ScholarWorks. It has been accepted for inclusion in VIMS Articles by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. 1 Salp contributions to vertical carbon flux in the Sargasso 2 Sea 3 4 5 Joshua P. Stonea,*, Deborah K. Steinberga 6 a Department of Biological Sciences, Virginia Institute of Marine Science, College of William & Mary, 7 PO Box 1346, Gloucester Point, VA 23062, USA 8 * Corresponding author. 9 E-mail addresses: [email protected] (J. Stone), [email protected] (D. Steinberg) 10 11 1 © 2016. This manuscript version is made available under the Elsevier user license http://www.elsevier.com/open-access/userlicense/1.0/ 12 Abstract 13 We developed a one-dimensional model to estimate salp contributions to vertical carbon flux at the 14 Bermuda Atlantic Time-series Study (BATS) site in the North Atlantic subtropical gyre for a 17-yr period 15 (April 1994 to December 2011). -
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 ...................................................... -
Balaenoptera Bonaerensis – Antarctic Minke Whale
Balaenoptera bonaerensis – Antarctic Minke Whale compared to B. bonaerensis. This smaller form, termed the “Dwarf” Minke Whale, may be genetically different from B. bonaerensis, and more closely related to the North Pacific Minke Whales, and thus has been classified B. acutorostrata (Wada et al. 1991; IWC 2001). This taxonomic position, although somewhat controversial, has been accepted by the Convention on International Trade in Endangered Species of Wild Fauna and Flora (CITES), and the Convention on Migratory Species (CMS). Assessment Rationale The current IWC global estimate of abundance of Antarctic Dr. Meike Scheidat Minke Whales is about 500,000 individuals. The abundance estimates declined from about 700,000 for the second circumpolar set of abundance survey cruises Regional Red List status (2016) Least Concern* (1985/86 to 1990/91) to about 500,000 for the third National Red List status (2004) Least Concern (1991/92 to 2003/04). Although this decline was not statistically significant, the IWC Scientific Committee does Reasons for change No change consider these results to reflect a change. However, Global Red List status (2008) Data Deficient whether this change is genuine or attributed to greater proportions of pack ice limiting the survey extent, has not TOPS listing (NEMBA) (2007) None yet been determined. More detailed results from an CITES listing (1986) Appendix I assessment model are available for the mid-Indian to the mid-Pacific region, and suggest that the population Endemic No increased to a peak in 1970 and then declined, with it *Watch-list Data being unclear whether this decline has levelled off or is still continuing past 2000. -
The Origins of Chordate Larvae Donald I Williamson* Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom
lopmen ve ta e l B Williamson, Cell Dev Biol 2012, 1:1 D io & l l o l g DOI: 10.4172/2168-9296.1000101 e y C Cell & Developmental Biology ISSN: 2168-9296 Research Article Open Access The Origins of Chordate Larvae Donald I Williamson* Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom Abstract The larval transfer hypothesis states that larvae originated as adults in other taxa and their genomes were transferred by hybridization. It contests the view that larvae and corresponding adults evolved from common ancestors. The present paper reviews the life histories of chordates, and it interprets them in terms of the larval transfer hypothesis. It is the first paper to apply the hypothesis to craniates. I claim that the larvae of tunicates were acquired from adult larvaceans, the larvae of lampreys from adult cephalochordates, the larvae of lungfishes from adult craniate tadpoles, and the larvae of ray-finned fishes from other ray-finned fishes in different families. The occurrence of larvae in some fishes and their absence in others is correlated with reproductive behavior. Adult amphibians evolved from adult fishes, but larval amphibians did not evolve from either adult or larval fishes. I submit that [1] early amphibians had no larvae and that several families of urodeles and one subfamily of anurans have retained direct development, [2] the tadpole larvae of anurans and urodeles were acquired separately from different Mesozoic adult tadpoles, and [3] the post-tadpole larvae of salamanders were acquired from adults of other urodeles. Reptiles, birds and mammals probably evolved from amphibians that never acquired larvae. -
Towards an Understanding of Salp Swarm Dynamics. ICES CM 2002/N
CM 2002/ N:12 Towards an understanding of salp swarm dynamics by Patricia Kremer ABSTRACT Species of salps are characterized by intermittent blooms. Several studies have documented the importance of physical processes both in providing seed stocks of salps and creating an environment that is favorable for the rapid increase of salp populations. Although salps are typically oceanic, most observations of bloom dynamics have been made in more accessible inshore waters, so it is difficult to assess how frequent and widespread these swarms are. A review and comparison of existing data is helping to define geographic “hot spots” for salp blooms as well as the necessary physical and biological precursors. Although at this point, the review is far from complete, several generalities are emerging. The details of the physical forcing functions vary, but the overall physical regime seems to require a region of pulsed mixing of oceanic water that results in a relatively high standing stock of autotrophs. For a salp bloom to occur, there also needs to be an adequate seed population of salps and sufficient sustained primary production to support the biomass of the salp population as the bloom develops. As non-selective filter feeders, salps are able to remove a wide range of particulates from the water column, transforming the undigested portion into fast sinking feces. Therefore, when salps occur at high densities, the water is characterized by low abundance of other plankton, with obvious trophic implications. Patricia Kremer: Marine Sciences, University of Connecticut, Groton CT 06340-6097, USA [tel: +1 860 405 9140; fax: +1 860 405 9153; e-mail [email protected]] INTRODUCTION Salps are holoplanktonic grazers that have a life history, feeding biology, and population dynamics that contrasts sharply to copepods and other crustacean zooplankton (Madin and Deibel 1998). -
The Secret Lives of JELLYFISH Long Regarded As Minor Players in Ocean Ecology, Jellyfish Are Actually Important Parts of the Marine Food Web
The secret lives of JELLYFISH Long regarded as minor players in ocean ecology, jellyfish are actually important parts of the marine food web. BY GARRY HAMILTON ennifer Purcell watches intently as the boom of the research ship Moon jellyfish (Aurelia Skookum slowly eases a 3-metre-long plankton net out of Puget Sound aurita) contain more Jnear Olympia, Washington. The marine biologist sports a rain suit, calories than some which seems odd for a sunny day in August until the bottom of the net other jellyfish. is manoeuvred in her direction, its mesh straining from a load of moon jellyfish (Aurelia aurita). Slime drips from the bulging net, and long ten- tacles dangle like a scene from an alien horror film. But it does not bother Purcell, a researcher at Western Washington University’s marine centre in Anacortes. Pushing up her sleeves, she plunges in her hands and begins to count and measure the messy haul with an assuredness borne from nearly 40 years studying these animals. 432 | NATURE | VOL 531 | 24 MARCH 2016 © 2016 Macmillan Publishers Limited. All rights reserved FEATURE NEWS Most marine scientists do not share her enthusiasm for the creatures. also inaccessible, living far out at sea or deep below the light zone. They Purcell has spent much of her career locked in a battle to find funding often live in scattered aggregations that are prone to dramatic popula- and to convince ocean researchers that jellyfish deserve attention. But tion swings, making them difficult to census. Lacking hard parts, they’re she hasn’t had much luck. -
Enormous Carnivores, Microscopic Food, and a Restaurant That's Hard to Find
Enormous Carnivores, Microscopic Food, and a Restaurant That's Hard to Find MARK F. BAUMGARTNER, CHARLES A. MAYO, AND ROBERT D. KENNEY April 1986 Cape Cod Bay We'd known for a long time that there were places east of Cape Cod where pow+l tidal impulses meet the sluggiih southward-moving coastal cur- rent, places where right whales lined up along the rips where plankton con- centrate. On a windless day in early April 1986, we decided to see ifright whales hadfoundsuch an area. The winter season, when right whales come to Cape Cod, had been a hard one, and calm hys like this were few, so we could at last get to the more distant convergence and, as localjshermen do, see what we could catch. It was gloomy and nearly dzrk when we lefi the port. For those of us who study whales, expectations are usually tempered by realip; we were lookingfor one of the rarest of all mammals in the shroud of the ocean. To- day, however, spirits were high as the hybreak was filed with springtime promise. Along the great outer beach of the Cape, so close to shore that we couldsmell the land nearb, thefist right whale was spotted working along one of those current rips. And as the sun climbed out of the haze, the whale rose and opened that great and odd mouth and skimmed the su$ace in a silence broken only ly the sizzle of water passing through its huge filtering Enormous Carnivores, Microscopic Food 139 apparatus. Our earlier optimism was warranted, andfor several hours we drzFedjust clear of the linear rip that the whale was working, recording the complex pattern of its movements. -
Dynamics of CO2 Evolution of Arctic Soils from Northern Siberia and Scandinavia
Dynamics of CO2 evolution of Arctic soils from Northern Siberia and Scandinavia Manfred Bölter*, Rolf Möller, Wiebke Müller-Lupp, and Nathalie Soethe Institute for Polar Ecology, University Kiel, Wischhofstr. 1-3, Bldg. 12, 24148 Kiel, Germany *Corresponding author: [email protected] 1. INTRODUCTION Growing interest in soil respiration in Arctic environments has opened wide research fields in microbial physiology and models associated therewith (Shivaji 2004). Much interest has been focused on metabolism in cold environments, with special emphasis on CO2 and CH4 evolution from tundra soils (Nadelhoffer et al. 1997, Vourlitis and Oechel 1997a,b). For modeling approaches, however, it is important to include the variability of microbial communities and their reactions to temperature shifts, i.e., the possible individual adaptations to temperature spans and related shifts in Q10 values of metabolic activity, which may indicate significant alterations in metabolic processes that point to important ecological factors to consider in the study of soil biological processes (Nadelhoffer et al. 1991, Sjögertsen and Wookey 2002). Special attention must be paid to processes at the cellular and subcellular level, and to the enzymes and substrates involved: an investigative effort that constitutes a crucial step in linking landscape modeling to small-scale processes. Soil carbon loss, generally termed soil respiration, is principally due to microbial and root respiration. Its measure can be defined in three ways (Haber 1958), i) the “physiological line”, ii) the “physical line”, and iii) the “ecological line”. The physiological line is mainly focused on the efficiency of soil organisms (and roots) and the reaction potential to the various environmental influences.