National Environmental Limits and Footprints Based on the Planetary
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A Model for the Oceanic Mass Balance of Rhenium and Implications for the Extent of Proterozoic Ocean Anoxia
UC Riverside UC Riverside Previously Published Works Title A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia Permalink https://escholarship.org/uc/item/1gh1h920 Journal GEOCHIMICA ET COSMOCHIMICA ACTA, 227 ISSN 0016-7037 Authors Sheen, Alex I Kendall, Brian Reinhard, Christopher T et al. Publication Date 2018-04-15 DOI 10.1016/j.gca.2018.01.036 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 227 (2018) 75–95 www.elsevier.com/locate/gca A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia Alex I. Sheen a,b,⇑, Brian Kendall a, Christopher T. Reinhard c, Robert A. Creaser b, Timothy W. Lyons d, Andrey Bekker d, Simon W. Poulton e, Ariel D. Anbar f,g a Department of Earth and Environmental Sciences, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada b Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada c School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA d Department of Earth Sciences, University of California, Riverside, CA 92521, USA e School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK f School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA g School of Molecular Sciences, Arizona State University, Tempe, AZ 85287, USA Received 13 July 2017; accepted in revised form 30 January 2018; available online 8 February 2018 Abstract Emerging geochemical evidence suggests that the atmosphere-ocean system underwent a significant decrease in O2 content following the Great Oxidation Event (GOE), leading to a mid-Proterozoic ocean (ca. -
Cascading of Habitat Degradation: Oyster Reefs Invaded by Refugee Fishes Escaping Stress
Ecological Applications, 11(3), 2001, pp. 764±782 q 2001 by the Ecological Society of America CASCADING OF HABITAT DEGRADATION: OYSTER REEFS INVADED BY REFUGEE FISHES ESCAPING STRESS HUNTER S. LENIHAN,1 CHARLES H. PETERSON,2 JAMES E. BYERS,3 JONATHAN H. GRABOWSKI,2 GORDON W. T HAYER, AND DAVID R. COLBY NOAA-National Ocean Service, Center for Coastal Fisheries and Habitat Research, 101 Pivers Island Road, Beaufort, North Carolina 28516 USA Abstract. Mobile consumers have potential to cause a cascading of habitat degradation beyond the region that is directly stressed, by concentrating in refuges where they intensify biological interactions and can deplete prey resources. We tested this hypothesis on struc- turally complex, species-rich biogenic reefs created by the eastern oyster, Crassostrea virginica, in the Neuse River estuary, North Carolina, USA. We (1) sampled ®shes and invertebrates on natural and restored reefs and on sand bottom to compare ®sh utilization of these different habitats and to characterize the trophic relations among large reef-as- sociated ®shes and benthic invertebrates, and (2) tested whether bottom-water hypoxia and ®shery-caused degradation of reef habitat combine to induce mass emigration of ®sh that then modify community composition in refuges across an estuarine seascape. Experimen- tally restored oyster reefs of two heights (1 m tall ``degraded'' or 2 m tall ``natural'' reefs) were constructed at 3 and 6 m depths. We sampled hydrographic conditions within the estuary over the summer to monitor onset and duration of bottom-water hypoxia/anoxia, a disturbance resulting from density strati®cation and anthropogenic eutrophication. Reduc- tion of reef height caused by oyster dredging exposed the reefs located in deep water to hypoxia/anoxia for .2 wk, killing reef-associated invertebrate prey and forcing mobile ®shes into refuge habitats. -
Son of Perdition Free Download
SON OF PERDITION FREE DOWNLOAD Wendy Alec | 490 pages | 01 Apr 2010 | Warboys Publishing (Ireland) Limited | 9780956333001 | English | Dublin, Ireland Who Is the Son of Perdition? The unembodied spirits who supported Lucifer in the war in heaven and were cast out Moses and mortals who commit Son of Perdition unpardonable sin against the Holy Ghost will inherit the same condition as Lucifer and Cain, and thus are called "sons of Son of Perdition. Contrasting beliefs. Recently Popular Media x. Verse Only. BLB Searches. So who is he? The bible describes the behavior of one who worships Jesus Christ. The purposes of the Son of Perdition oppose those of Jesus. A verification email has been sent to the address you provided. Blue Letter Bible study tools make reading, Son of Perdition and studying the Bible easy and rewarding. Extinction event Holocene extinction Human extinction List of extinction events Genetic erosion Son of Perdition pollution. Christianity portal. Re-type Password. Even a believer who maintains the faith can become discouraged and lose the peace of the Holy Spirit when he is cut off from the body of Christ. Biblical texts. By proceeding, you consent to our cookie usage. Back Psalms 1. The Son of Perdition is the progeny of abuse and desolation. Sort Canonically. The Millennium. No Number. Advanced Options Exact Match. However, scripture declares that "the soul can never die" Son of Perdition and that in the Resurrection the spirit and the body are united "never to be divided" Alma ; cf. Individual instructors or editors may still require Son of Perdition use of URLs. -
Substantial Vegetation Response to Early Jurassic Global Warming with Impacts on Oceanic Anoxia
ARTICLES https://doi.org/10.1038/s41561-019-0349-z Substantial vegetation response to Early Jurassic global warming with impacts on oceanic anoxia Sam M. Slater 1*, Richard J. Twitchett2, Silvia Danise3 and Vivi Vajda 1 Rapid global warming and oceanic oxygen deficiency during the Early Jurassic Toarcian Oceanic Anoxic Event at around 183 Ma is associated with a major turnover of marine biota linked to volcanic activity. The impact of the event on land-based eco- systems and the processes that led to oceanic anoxia remain poorly understood. Here we present analyses of spore–pollen assemblages from Pliensbachian–Toarcian rock samples that record marked changes on land during the Toarcian Oceanic Anoxic Event. Vegetation shifted from a high-diversity mixture of conifers, seed ferns, wet-adapted ferns and lycophytes to a low-diversity assemblage dominated by cheirolepid conifers, cycads and Cerebropollenites-producers, which were able to sur- vive in warm, drought-like conditions. Despite the rapid recovery of floras after Toarcian global warming, the overall community composition remained notably different after the event. In shelf seas, eutrophication continued throughout the Toarcian event. This is reflected in the overwhelming dominance of algae, which contributed to reduced oxygen conditions and to a marked decline in dinoflagellates. The substantial initial vegetation response across the Pliensbachian/Toarcian boundary compared with the relatively minor marine response highlights that the impacts of the early stages of volcanogenic -
Effects of Natural and Human-Induced Hypoxia on Coastal Benthos
Biogeosciences, 6, 2063–2098, 2009 www.biogeosciences.net/6/2063/2009/ Biogeosciences © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Effects of natural and human-induced hypoxia on coastal benthos L. A. Levin1, W. Ekau2, A. J. Gooday3, F. Jorissen4, J. J. Middelburg5, S. W. A. Naqvi6, C. Neira1, N. N. Rabalais7, and J. Zhang8 1Integrative Oceanography Division, Scripps Institution of Oceanography, 9500 Gilman Drive, La Jolla, CA 92093-0218, USA 2Fisheries Biology, Leibniz Zentrum fur¨ Marine Tropenokologie,¨ Leibniz Center for Tropical Marine Ecology, Fahrenheitstr. 6, 28359 Bremen, Germany 3National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK 4Laboratory of Recent and Fossil Bio-Indicators (BIAF), Angers University, 2 Boulevard Lavoisier, 49045 Angers Cedex 01, France 5Faculty of Geosciences, Utrecht University, P.O. Box 80021, 3508 TA Utrecht, The Netherlands 6National Institution of Oceanography, Dona Paula, Goa 403004, India 7Louisiana Universities Marine Consortium, Chauvin, Louisiana 70344, USA 8State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 3663 Zhongshan Road North, Shanghai 200062, China Received: 17 January 2009 – Published in Biogeosciences Discuss.: 3 April 2009 Revised: 21 August 2009 – Accepted: 21 August 2009 – Published: 8 October 2009 Abstract. Coastal hypoxia (defined here as <1.42 ml L−1; Mobile fish and shellfish will migrate away from low-oxygen 62.5 µM; 2 mg L−1, approx. 30% oxygen saturation) devel- areas. Within a species, early life stages may be more subject ops seasonally in many estuaries, fjords, and along open to oxygen stress than older life stages. coasts as a result of natural upwelling or from anthropogenic Hypoxia alters both the structure and function of benthic eutrophication induced by riverine nutrient inputs. -
Powering a Sustainable and Circular Economy— an Engineering Approach to Estimating Renewable Energy Potentials Within Earth System Boundaries
energies Article Powering a Sustainable and Circular Economy— An Engineering Approach to Estimating Renewable Energy Potentials within Earth System Boundaries Harald Desing * , Rolf Widmer , Didier Beloin-Saint-Pierre and Roland Hischier and Patrick Wäger Empa – Swiss Federal Laboratories for Materials Science and Technology, Lerchenfeldstrasse 5, CH-9014 St.Gallen, Switzerland; [email protected] (R.W.); [email protected] (D.B.-S.-P.); [email protected] (R.H.); [email protected] (P.W.) * Correspondence: [email protected] Received: 30 October 2019; Accepted: 4 December 2019; Published: 11 December 2019 Abstract: This study proposes a method to estimate the appropriability of renewable energy resources at the global scale, when Earth system boundaries/needs and the human demand for chemical energy are respected. The method is based on an engineering approach, i.e., uncertainties of parameters and models are considered and potentials calculated with 99% confidence. We used literature data to test our method and provide initial results for global appropriable technical potentials (ATP) that sum up to 71 TW, which is significantly larger than the current global energy demand. Consequently, there is sufficient renewable energy potentially available to increase energy access for a growing world population as well as for a development towards increasingly closed material cycles within the technosphere. Solar energy collected on the built environment (29%) and in desert areas (69%) represent the dominant part of this potential, followed in great distance by hydro (0.6%), terrestrial heat (0.4%), wind (0.35%), and biomass (0.2%). Furthermore, we propose indicators to evaluate an energy mix on different levels, from an energy mix in single products to the mix used by the global economy, against the estimated RE potentials, which allow an evaluation and consideration in the design of sustainable–circular products and systems. -
Slow-Onset Processes and Resulting Loss and Damage
Publication Series ADDRESSING LOSS AND DAMAGE FROM SLOW-ONSET PROCESSES Slow-onset Processes and Resulting Loss and Damage – An introduction Table of contents L 4 22 ist of a bbre Summary of Loss and damage via tio key facts and due to slow-onset ns definitions processes AR4 IPCC Fourth Assessment Report 6 22 What is loss and damage? Introduction AR5 IPCC Fifth Assessment Report COP Conference of the Parties to the 23 United Nations Framework Convention on 9 What losses and damages IMPRINT Climate Change can result from slow-onset Slow-onset ENDA Environment Development Action Energy, processes? Authors Environment and Development Programme processes and their Laura Schäfer, Pia Jorks, Emmanuel Seck, Energy key characteristics 26 Oumou Koulibaly, Aliou Diouf ESL Extreme Sea Level What losses and damages Contributors GDP Gross Domestic Product 9 can result from sea level rise? Idy Niang, Bounama Dieye, Omar Sow, Vera GMSL Global mean sea level What is a slow-onset process? Künzel, Rixa Schwarz, Erin Roberts, Roxana 31 Baldrich, Nathalie Koffi Nguessan GMSLR Global mean sea level rise 10 IOM International Organization on Migration What are key characteristics Loss and damage Editing Adam Goulston – Scize Group LLC of slow-onset processes? in Senegal due to IPCC Intergovernmental Panel on Climate Change sea level rise Layout and graphics LECZ Low-elevation coastal zone 14 Karin Roth – Wissen in Worten OCHA Office for the Coordination of Humanitarian Affairs What are other relevant January 2021 terms for the terminology on 35 RCP Representative -
Ecosystems Mario V
Ecosystems Mario V. Balzan, Abed El Rahman Hassoun, Najet Aroua, Virginie Baldy, Magda Bou Dagher, Cristina Branquinho, Jean-Claude Dutay, Monia El Bour, Frédéric Médail, Meryem Mojtahid, et al. To cite this version: Mario V. Balzan, Abed El Rahman Hassoun, Najet Aroua, Virginie Baldy, Magda Bou Dagher, et al.. Ecosystems. Cramer W, Guiot J, Marini K. Climate and Environmental Change in the Mediterranean Basin -Current Situation and Risks for the Future, Union for the Mediterranean, Plan Bleu, UNEP/MAP, Marseille, France, pp.323-468, 2021, ISBN: 978-2-9577416-0-1. hal-03210122 HAL Id: hal-03210122 https://hal-amu.archives-ouvertes.fr/hal-03210122 Submitted on 28 Apr 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Climate and Environmental Change in the Mediterranean Basin – Current Situation and Risks for the Future First Mediterranean Assessment Report (MAR1) Chapter 4 Ecosystems Coordinating Lead Authors: Mario V. Balzan (Malta), Abed El Rahman Hassoun (Lebanon) Lead Authors: Najet Aroua (Algeria), Virginie Baldy (France), Magda Bou Dagher (Lebanon), Cristina Branquinho (Portugal), Jean-Claude Dutay (France), Monia El Bour (Tunisia), Frédéric Médail (France), Meryem Mojtahid (Morocco/France), Alejandra Morán-Ordóñez (Spain), Pier Paolo Roggero (Italy), Sergio Rossi Heras (Italy), Bertrand Schatz (France), Ioannis N. -
Uranium Isotope Evidence for Two Episodes of Deoxygenation During Oceanic Anoxic Event 2
Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2 Matthew O. Clarksona,1,2, Claudine H. Stirlinga, Hugh C. Jenkynsb, Alexander J. Dicksonb,c, Don Porcellib, Christopher M. Moyd, Philip A. E. Pogge von Strandmanne, Ilsa R. Cookea, and Timothy M. Lentonf aDepartment of Chemistry, University of Otago, Dunedin 9054, New Zealand; bDepartment of Earth Sciences, University of Oxford, Oxford OX1 3AN, United Kingdom; cDepartment of Earth Sciences, Royal Holloway University of London, Egham TW20 0EX, United Kingdom; dDepartment of Geology, University of Otago, Dunedin 9054, New Zealand; eLondon Geochemistry and Isotope Centre, Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, London WC1E 6BT, United Kingdom; and fEarth System Science, College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4QE, United Kingdom Edited by Thure E. Cerling, University of Utah, Salt Lake City, UT, and approved January 22, 2018 (received for review August 30, 2017) Oceanic Anoxic Event 2 (OAE 2), occurring ∼94 million years ago, successions in many ocean basins. The preferential burial of iso- was one of the most extreme carbon cycle and climatic perturba- topically light carbon (C) also contributed to a broad positive carbon tions of the Phanerozoic Eon. It was typified by a rapid rise in isotope excursion (CIE) across OAE 2 that is utilized as a global atmospheric CO2, global warming, and marine anoxia, leading to chemostratigraphic marker of the event (1). Silicate weathering and the widespread devastation of marine ecosystems. However, the organic carbon burial are vital components of the global carbon cycle precise timing and extent to which oceanic anoxic conditions ex- and represent important negative feedback mechanisms that se- panded during OAE 2 remains unresolved. -
Four of Nine 'Planetary Boundaries' Exceeded
Four of nine ‘planetary boundaries’ exceeded Civilisation has crossed four of nine ‘planetary boundaries’, increasing the risk of irreversibly driving the Earth in to a less hospitable state, concludes new research. These are: extinction rate, deforestation, atmospheric CO2 and the flow of nitrogen and phosphorus. 16 April 2015 Issue 410 Planetary boundaries are scientifically based levels of human pressure on critical global Subscribe to free processes that could create irreversible and abrupt change to the ‘Earth System’ — the weekly News Alert complex interaction of atmosphere, ice caps, sea, land and biota. These boundaries were first identified and put forward by scientists in 2009. They help decision makers by defining Source: Steffen, W., Richardson, K., Rockström, a safe operating space for humanity. J., Cornell, S.E., Fetzer, I., Crossing planetary boundaries increases the risk of moving the Earth System to a state Bennett, E.M., Biggs, R., much less hospitable for human civilisation than the one in which we have flourished in over Carpenter, S.R., de Vries, the past 11 000 years (the ‘Holocene epoch’). W., de Wit, C.A., Folke, C., Gerten, D., Heinke, J., Planetary boundaries represent a precautionary approach, based on maintaining a Holocene- Mace, G.M., Persson, L.M., like state of the Earth System. Beyond each boundary is a ‘zone of uncertainty’, where there Ramanathan, V., Reyers, is an increased risk of outcomes that are damaging to human wellbeing. Taken together the B., & Sörlin, S. (2015). boundaries define a safe operating space for humanity. Approaching a boundary provides a Planetary boundaries: warning signal to decision makers, indicating that we are approaching a problem while Guiding human allowing time for corrective action before it is too late. -
Ocean Acidification in Washington State
University of Washington • Washington Sea Grant Ocean Acidification in Washington State What is Ocean Acidification? OA in Washington State cean Acidification (or ‘OA’) is a long-term decrease ur region is experiencing ocean acidification sooner Oin seawater pH that is primarily caused by the Oand more severely than expected, due to a combina- ocean’s uptake of carbon dioxide (CO2 ) from the atmo- tion of human and natural causes. In the spring and sum- sphere. CO2 generated by humans’ use of fossil fuels and mer, acidification along our coast is compounded by up- deforestation has been accumulating in the atmosphere welling, which mixes deep, naturally low-pH seawater into since the industrial revolution. About one quarter of this the already acidified surface layer. In Puget Sound, nutri- CO2 is absorbed by the oceans, pH describes the acidity of a liquid ents generated by human activities (mostly where it reacts with water to form nitrogen and phosphorus from sewage, carbonic acid. As a result, the aver- fertilizers and manure) fuel processes that age pH of seawater at the ocean add even more CO2 to this ‘doubly-acidified’ surface has already dropped by ~0.1 seawater. The combination can be deadly units, a 30% increase in acidity. If to vulnerable organisms. pH levels as low atmospheric CO2 levels continue as 7.4 have been recorded in Hood Canal, to climb at the present rate, ocean an important shellfish-growing region. acidity will double by the end of this State and federal agencies, scientists, tribes, century. shellfish growers and NGOs are working together to address OA in our region. -
Governing Planetary Boundaries: Limiting Or Enabling Conditions for Transitions Towards Sustainability?
Chapter 5 Governing Planetary Boundaries: Limiting or Enabling Conditions for Transitions Towards Sustainability? Falk Schmidt Abstract It seems intuitive to identify boundaries of an earth system which is increasingly threatened by human activities. Being aware of and hence studying boundaries may be necessary for effective governance of sustainable development. Can the planetary boundaries function as useful ‘warning signs’ in this respect? The answer presented in the article is: yes; but. It is argued that these boundaries cannot be described exclusively by scientific knowledge-claims. They have to be identified by science-society or transdisciplinary deliberations. The discussion of governance challenges related to the concept concludes with two main recommendations: to better institutionalise integrative transdisciplinary assessment processes along the lines of the interconnected nature of the planetary boundaries, and to foster cross- sectoral linkages in order to institutionalise more integrative and yet context sensitive governance arrangements. These insights are briefly confronted with options for institutional reform in the context of the Rio + 20 process. If humankind will not manage a transition towards sustainability, its ‘safe operating space’ continues shrinking. Governance arrangements for such ‘systems at risk’ may then be, first, more ‘forceful’ and, second, may run counter to our understanding of ‘open societies’. It is not very realistic that the world is prepared to achieve the first, and it is not desirable to get the effects of the latter. Scholars and practitioners of sustainability may find this a convincing argument to act now. 5.1 Targets The two-degree target concerning climate change has been vigorously debated during the run-up to and the aftermath of the Copenhagen Climate Conference COP 15 (WBGU 2009; Berkhout 2010; Geden 2010; Hulme 2010a; Jaeger and F.