The Ocean Biosphere: from Microbes to Mammals
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Preliminary Catalog of the Sedimentary Basins of the United States
Preliminary Catalog of the Sedimentary Basins of the United States By James L. Coleman, Jr., and Steven M. Cahan Open-File Report 2012–1111 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Coleman, J.L., Jr., and Cahan, S.M., 2012, Preliminary catalog of the sedimentary basins of the United States: U.S. Geological Survey Open-File Report 2012–1111, 27 p. (plus 4 figures and 1 table available as separate files) Available online at http://pubs.usgs.gov/of/2012/1111/. iii Contents Abstract ...........................................................................................................................................................1 -
Energy Budget of the Biosphere and Civilization: Rethinking Environmental Security of Global Renewable and Non-Renewable Resources
ecological complexity 5 (2008) 281–288 available at www.sciencedirect.com journal homepage: http://www.elsevier.com/locate/ecocom Viewpoint Energy budget of the biosphere and civilization: Rethinking environmental security of global renewable and non-renewable resources Anastassia M. Makarieva a,b,*, Victor G. Gorshkov a,b, Bai-Lian Li b,c a Theoretical Physics Division, Petersburg Nuclear Physics Institute, Russian Academy of Sciences, 188300 Gatchina, St. Petersburg, Russia b CAU-UCR International Center for Ecology and Sustainability, University of California, Riverside, CA 92521, USA c Ecological Complexity and Modeling Laboratory, Department of Botany and Plant Sciences, University of California, Riverside, CA 92521-0124, USA article info abstract Article history: How much and what kind of energy should the civilization consume, if one aims at Received 28 January 2008 preserving global stability of the environment and climate? Here we quantify and compare Received in revised form the major types of energy fluxes in the biosphere and civilization. 30 April 2008 It is shown that the environmental impact of the civilization consists, in terms of energy, Accepted 13 May 2008 of two major components: the power of direct energy consumption (around 15 Â 1012 W, Published on line 3 August 2008 mostly fossil fuel burning) and the primary productivity power of global ecosystems that are disturbed by anthropogenic activities. This second, conventionally unaccounted, power Keywords: component exceeds the first one by at least several times. Solar power It is commonly assumed that the environmental stability can be preserved if one Hydropower manages to switch to ‘‘clean’’, pollution-free energy resources, with no change in, or Wind power even increasing, the total energy consumption rate of the civilization. -
Bottom Water and Bottom Configuration of the Great Atlantic Deeps. (1) (2)
bOTTOM WATER AND bOTTOM CONFIGURATION OF THE GREAT ATLANTIC DEEPS. (1) (2). (Extract from the Results of the German Atlantic Expedition) by G e o r g WUST. The problem of the origin and distribution of bottom water has been discussed from early times, and often. This results from the fact that more abundant materials of observation exist for the bottom than for the deep layers, because measurements of bottom temperature have been taken not only by exploring vessels, but also by hydro- graphic and cable-laying ships. The remarkably low temperatures of nearly o° C. on the bottom, which were confirmed on each occasion, also early served as the principal foun dation of the hypothesis of the polar origin of the bottom water. The polar bottom currents are consequently members of the deep oceanic circulation, the existence of which had been deduced from the distribution of the temperature before the Challenger expedi tion. If it had been thought before that time that the Arctic and Antarctic currents showed roughly the same development and met at the equator, it became clear, after the Challenger and Gazelle observations, that the principal mass of the bottom waters of the great oceans comes from the Antarctic Basin ; that in the Atlantic Ocean this bottom current chiefly leads into the western trough ; and that it can still be detected in the form of a cold stream as far as the equator (in its last ramifications it even passes the equator and reaches the North Atlantic). These expeditions have also shown the value of bottom temperatures for revealing the first magnitude shapes of the ocean bottom, a value which has been proved for the Atlantic Ocean by two examples which have become classic. -
Kinematics and Extent of the Piemont-Liguria Basin
https://doi.org/10.5194/se-2020-161 Preprint. Discussion started: 8 October 2020 c Author(s) 2020. CC BY 4.0 License. Kinematics and extent of the Piemont-Liguria Basin – implications for subduction processes in the Alps Eline Le Breton1, Sascha Brune2,3, Kamil Ustaszewski4, Sabin Zahirovic5, Maria Seton5, R. Dietmar Müller5 5 1Department of Earth Sciences, Freie Universität Berlin, Germany 2Geodynamic Modelling Section, German Research Centre for Geosciences, GFZ Potsdam, Germany 3Institute of Geosciences, University of Potsdam, Potsdam, Germany 4Institute for Geological Sciences, Friedrich-Schiller-Universität Jena, Germany 10 5EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia Correspondence to: Eline Le Breton ([email protected]) Abstract. Assessing the size of a former ocean, of which only remnants are found in mountain belts, is challenging but crucial to understand subduction and exhumation processes. Here we present new constraints on the opening and width of the Piemont- Liguria (PL) Ocean, known as the Alpine Tethys together with the Valais Basin. We use a regional tectonic reconstruction of 15 the Western Mediterranean-Alpine area, implemented into a global plate motion model with lithospheric deformation, and 2D thermo-mechanical modelling of the rifting phase to test our kinematic reconstructions for geodynamic consistency. Our model fits well with independent datasets (i.e. ages of syn-rift sediments, rift-related fault activity and mafic rocks) and shows that the PL Basin opened in four stages: (1) Rifting of the proximal continental margin in Early Jurassic (200-180 Ma), (2) Hyper- extension of the distal margin in Early-Middle Jurassic (180-165 Ma), (3) Ocean-Continent Transition (OCT) formation with 20 mantle exhumation and MORB-type magmatism in Middle-Late Jurassic (165-154 Ma), (4) Break-up and “mature” oceanic spreading mostly in Late Jurassic (154-145 Ma). -
For-75: an Ecosystem Approach to Natural Resources Management
FOR-75 An Ecosystems Approach to Natural Resources Management Thomas G. Barnes, Extension Wildlife Specialist ur nation—and especially Kentucky—has an The glade cress Oabundance of renewable natural resources, including timber, wildlife, and water. These re- sources have allowed us to build a strong nation and economy, creating one of the highest stan- dards of living in the world. As our nation grew and prospered during the past 200 years, we ex- tracted those natural resources through agricul- ture, forestry, mining, urban or industrial expansion, and other developments. Ultimately, we affected the amount of wild lands that native plants and animals need for survival. In the past, natural resources agencies have ral- The glade cress grows in Jefferson and Bullitt counties lied public support for declining wildlife popula- and nowhere else in the world. tions. In the 1930s, Congress passed the Federal Aid to Wildlife Resto- Table 1. Selected Ecosystem Declines in the ration Act, also called including the bald eagle, brown pelican, peregrine United States the Pittman-Robertson falcon, and American alligator, have recovered % Decline (loss) or Act, and state wildlife from the brink of extinction. However, numerous Ecosystem or Community Degradation agencies received fund- other species and unique habitats are declining, Pacific Northwest Old Growth Forest 90 ing to restore numerous and the list of endangered and threatened organ- Northeastern Pine Barrens 48 wildlife species that isms continues to grow every year. Why are these Tall Grass Prairie 961 were in trouble, includ- additional species in trouble, while other species Palouse Prairie 98 ing white-tailed deer, are increasing their populations and ranges? Where did we go wrong? Why, almost immedi- Blackbelt Prairies 98 wild turkeys, wood ducks, elk, and prong- ately after passage of the Endangered Species Act, Midwestern Oak Savanna 981 horn antelope. -
Biosphere Introduction the Biosphere in Education
10/5/2016 Biosphere Encyclopedia of Earth AUTHOR LOGIN EOE PAGES BROWSE THE EOE Home Article Tools: Titles (AZ) About the EoE Authors Editorial Board Biosphere Topics International Advisory Board Topic Editors FAQs Lead Author: Erle Ellis (other articles) Content Partners EoE for Educators Article Topic: Geography Content Sources Contribute to the EoE This article has been reviewed and approved by the following Topic Editor: Leszek A. eBooks Bledzki (other articles) Support the EoE Classics Last Updated: January 8, 2009 Contact the EoE Collections Find Us Here RSS Reviews Table of Contents Awards and Honors Introduction 1 Introduction The biosphere is the biological component of earth systems, which 1.1 History of the Biosphere also include the lithosphere, hydrosphere, atmosphere and other Concept 2 The Biosphere in Education "spheres" (e.g. cryosphere, anthrosphere, etc.). The biosphere 3 Biosphere Research includes all living organisms on earth, together with the dead organic 4 The Future of the Biosphere matter produced by them. 5 More About the Biosphere 6 Further Reading The biosphere concept is common to many scientific disciplines including astronomy, SOLUTIONS JOURNAL geophysics, geology, hydrology, biogeography and evolution, and is a core concept in ecology, earth science and physical geography. A key component of earth systems, the biosphere interacts with and exchanges matter and energy with the other spheres, helping to drive the global biogeochemical cycling of carbon, nitrogen, phosphorus, sulfur and other elements. From an ecological point of view, the biosphere is the "global ecosystem", comprising the totality of biodiversity on earth and performing all manner of biological functions, including photosynthesis, respiration, decomposition, nitrogen fixation and denitrification. -
The Biosphere Reserve Program in the United States
tions recommending widespread phosphorus 15. For example, T. P. Murphy, D. R. S. Lean, visualize a laboratory bioassay experi- control as a solution to eutrophication. Almost and C. Nalewajko [Science 192, 900 (1976)] ment that could realistically represent all all of the freshwater scientists in the world were showed that Anabaena requires iron for fixation represented. of atmospheric nitrogen and that this genus of these parameters. 3. For example, see J. W. G. Lund [Nature (Lon- can suppress the growth of other species of On the basis of data from several don) 249, 797 (1974)] for a critique of phos- algae by excretion of a growth-inhibiting phorus control, including my report of the same substance. studies of the carbon, nitrogen, and year (4). 16. M. Turner and R. Flett, unpublished data. As 4. D. W. Schindler, Science 184, 897 (1974). yet no quantitative estimates of nitrogen fixation phosphorus cycle, I hypothesize that 5. P. Dillon and F. Rigler,J. Fish. Res. Board Can. for an entire season are available. G. Persson, S. schemes for controlling nitrogen input to 32, 1519 (1975); R. A. Vollenweider, Schweiz. Z. K. Holmgren, M. Jansson, A. Lundgren, and C. Hydrol. 37, 53 (1975); D. W. Schindler, Limnol. Anell [in Proceedings of the NRC-CNC lakes may actually affect water quality Oceanogr., in press. (SCOPE) Circumpolar Conference on Northern adversely by causing low N/P ratios, 6. See papers in G. E. Likens, Ed., Am. Soc. Ecology (Ottawa, 15 to 18 September 1975)] Limnol. Oceanogr. Spec. Symp. No. 1 (1972). reported similar results for a lake in Sweden that which favor the vacuolate, nitrogen-fix- 7. -
UNIVERSITY of CALIFORNIA, SAN DIEGO Marine Geophysical Study
UNIVERSITY OF CALIFORNIA, SAN DIEGO Marine Geophysical Study of Cyclic Sedimentation and Shallow Sill Intrusion in the Floor of the Central Gulf of California A dissertation submitted in partial satisfaction of the requirements for the degree Doctor of Philosophy in Oceanography by Jared W. Kluesner Committee in Charge: Professor Peter Lonsdale, Chair Professor Paterno Castillo Professor Graham Kent Professor Falko Kuester Professor Michael Tryon Professor Edward Winterer 2011 Copyright Jared Kluesner, 2011 All rights reserved. The Dissertation of Jared W. Kluesner is approved, and it is acceptable in quality and in form for publication on microfilm and electronically: Chair University of California, San Diego 2011 iii To my parents, Tony and Donna Kluesner and my grandfather James Kluesner iv "...Let us go, we said, into the Sea of Cortez, realizing that we become forever a part of it" The Log from the Sea of Cortez John Steinbeck v TABLE OF CONTENTS Signature Page ...................................................................................... iii Dedication.............................................................................................. iv Epigraph ................................................................................................ v Table of Contents .................................................................................. vi List of Figures ........................................................................................ ix Acknowledgments ................................................................................ -
The 18.6Year Lunar Nodal Cycle and Surface Temperature Variability In
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, C02002, doi:10.1029/2006JC003671, 2007 The 18.6-year lunar nodal cycle and surface temperature variability in the northeast Pacific Stewart M. McKinnell1 and William R. Crawford2 Received 27 April 2006; revised 24 August 2006; accepted 21 September 2006; published 2 February 2007. [1] The 18.6-year lunar nodal cycle (LNC) is a significant feature of winter (January) air and sea temperatures along the North American west coast over a 400-year period. Yet much of the recent temperature variation can also be explained by wind patterns associated with the PNA teleconnection. At Sitka, Alaska, (57°N) and nearby stations in northern British Columbia, the January PNA index accounts for over 70% of average January air temperatures in lengthy meteorological records. It appears that the LNC signal in January air temperatures in this region is not independent of the PNA, but is a component of it. The Sitka air temperature record, along with SSTs along the British Columbia coast and the PNA index have significant cross-correlations with the LNC that appear at a 2-year lag, LNC leading. The influence of the PNA pattern declines in winter with decreasing latitude but the LNC component does not. It appears as a significant feature of long-term SST variation at Scripps Pier and the California Current System. The LNC also appears over centennial-scales in proxy temperatures along western North America. The linkage of LNC-moderated surface temperatures to processes involving basin-scale teleconnections expands the possibility that the proximate mechanism may be located remotely from its expression in the northeast Pacific. -
Biosphere Reserves' Management Effectiveness—A Systematic
sustainability Review Biosphere Reserves’ Management Effectiveness—A Systematic Literature Review and a Research Agenda Ana Filipa Ferreira 1,2,* , Heike Zimmermann 3, Rui Santos 1 and Henrik von Wehrden 2 1 CENSE—Center for Environmental and Sustainability Research, NOVA College of Science and Technology, NOVA University Lisbon, 2829-516 Caparica, Portugal; [email protected] 2 Institute of Ecology, Faculty of Sustainability and Center for Methods, Leuphana University, 21335 Lüneburg, Germany; [email protected] 3 Institute for Ethics and Transdisciplinary Sustainability Research, Faculty of Sustainability, Leuphana University, 21335 Lüneburg, Germany; [email protected] * Correspondence: [email protected]; Tel.: +351-21-294-8397 Received: 10 June 2020; Accepted: 2 July 2020; Published: 8 July 2020 Abstract: Research about biosphere reserves’ management effectiveness can contribute to better understanding of the existing gap between the biosphere reserve concept and its implementation. However, there is a limited understanding about where and how research about biosphere reserves’ management effectiveness has been conducted, what topics are investigated, and which are the main findings. This study addresses these gaps in the field, building on a systematic literature review of scientific papers. To this end, we investigated characteristics of publications, scope, status and location of biosphere reserves, research methods and management effectiveness. The results indicate that research is conceptually and methodologically diverse, but unevenly distributed. Three groups of papers associated with different goals of biosphere reserves were identified: capacity building, biodiversity conservation and sustainable development. In general, each group is associated with different methodological approaches and different regions of the world. The results indicate the importance of scale dynamics and trade-offs between goals, which are advanced as important leverage points for the success of biosphere reserves. -
Wilderness-Now More Than Ever a Response to Callicott
WILDERNESS-NOW MORE THAN EVER A RESPONSE TO CALLICOTT REED F. Noss (1994) J. Baird Callicott's "A Critique ofand an Alternative to the Wilderness Idea" is peculiar. It is nicely written and erudite, and it definitely pro vokes thought. But it also provokes, at least in me, a good deal offrus tration. Many ofus in the conservation movement have worked hard for years to promote ecological and evolutionary understanding as the logical foundation for land conservation (land in the sense Aldo Leopold used it, including air, soil, water, and biota), but coupled with the aesthetic and ethical appreciation ofwild things and wild places for their own sakes.Following Leopold, we have tried to unite brain and heart, rationality and intuition, in the struggle to defend wild nature. Yet here comes Callicott, a leading environmental ethicist, a Leopold scholar, a professed lover ofwildness, mounting an attack on the con cept ofwilderness. This article is only the latest in a series ofessays in which Callicott assails the idea ofwilderness as anachronistic, ecologi cally uninformed, ethnocentric, historically naive, and politically counterproductive. I believe Callicott is dead wrong and I will try to tell you why. First, I must state emphatically that I agree with much of Callicott's essay. His progressive interpretations ofbiosphere reserves, buffer zones, transition zones, sustainable livelihood, and ecological management are all in line with what I and many others affiliated with the Wildlands Project have supported and proposed. But Callicott portrays all these integrative concepts as alternatives to wilderness pro tection, as things conservationists should spend their time on instead 187 ofdefending wildlands. -
OCEAN SUBDUCTION Show That Hardly Any Commercial Enhancement Finney B, Gregory-Eaves I, Sweetman J, Douglas MSV Program Can Be Regarded As Clearly Successful
1982 OCEAN SUBDUCTION show that hardly any commercial enhancement Finney B, Gregory-Eaves I, Sweetman J, Douglas MSV program can be regarded as clearly successful. and Smol JP (2000) Impacts of climatic change and Model simulations suggest, however, that stock- Rshing on PaciRc salmon over the past 300 years. enhancement may be possible if releases can be Science 290: 795}799. made that match closely the current ecological Giske J and Salvanes AGV (1999) A model for enhance- and environmental conditions. However, this ment potentials in open ecosystems. In: Howell BR, Moksness E and Svasand T (eds) Stock Enhancement requires improvements of assessment methods of and Sea Ranching. Blackwell Fishing, News Books. these factors beyond present knowledge. Marine Howell BR, Moksness E and Svasand T (1999) Stock systems tend to have strong nonlinear dynamics, Enhancement and Sea Ranching. Blackwell Fishing, and unless one is able to predict these dynamics News Books. over a relevant time horizon, release efforts are Kareiva P, Marvier M and McClure M (2000) Recovery not likely to increase the abundance of the target and management options for spring/summer chinnook population. salmon in the Columbia River basin. Science 290: 977}979. Mills D (1989) Ecology and Management of Atlantic See also Salmon. London: Chapman & Hall. Ricker WE (1981) Changes in the average size and Mariculture, Environmental, Economic and Social average age of PaciRc salmon. Canadian Journal of Impacts of. Salmonid Farming. Salmon Fisheries: Fisheries and Aquatic Science 38: 1636}1656. Atlantic; Paci\c. Salmonids. Salvanes AGV, Aksnes DL, FossaJH and Giske J (1995) Simulated carrying capacities of Rsh in Norwegian Further Reading fjords.