Simple Stochastic Populations in Habi- Tats with Bounded, and Varying Carry- Ing Capacities
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Species Extinctions
http://www.iucn.org/about/union/commissions/wcpa/?7695/Multiple-ocean-stresses- threaten-globally-significant-marine-extinction Multiple ocean stresses threaten “globally significant” marine extinction 20 June 2011 | News story An international panel of experts warns in a report released today that marine species are at risk of entering a phase of extinction unprecedented in human history. The preliminary report arises from a ‘State of the Oceans’ workshop co-hosted by IUCN in April, the first ever to consider the cumulative impact of all pressures on the oceans. Considering the latest research across all areas of marine science, the workshop examined the combined effects of pollution, acidification, ocean warming, over-fishing and hypoxia (deoxygenation). The scientific panel concluded that the combination of stresses on the ocean is creating the conditions associated with every previous major extinction of species in Earth’s history. And the speed and rate of degeneration in the ocean is far greater than anyone has predicted. The panel concluded that many of the negative impacts previously identified are greater than the worst predictions. As a result, although difficult to assess, the first steps to globally significant extinction may have begun with a rise in the extinction threat to marine species such as reef- forming corals. “The world’s leading experts on oceans are surprised by the rate and magnitude of changes we are seeing,” says Dan Laffoley, Marine Chair of IUCN’s World Commission on Protected Areas, Senior Advisor on Marine Science and Conservation for IUCN and co-author of the report. “The challenges for the future of the ocean are vast, but unlike previous generations, we know what now needs to happen. -
What Is a Population? an Empirical Evaluation of Some Genetic Methods for Identifying the Number of Gene Pools and Their Degree of Connectivity
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Publications, Agencies and Staff of the U.S. Department of Commerce U.S. Department of Commerce 2006 What is a population? An empirical evaluation of some genetic methods for identifying the number of gene pools and their degree of connectivity Robin Waples NOAA, [email protected] Oscar Gaggiotti Université Joseph Fourier, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/usdeptcommercepub Waples, Robin and Gaggiotti, Oscar, "What is a population? An empirical evaluation of some genetic methods for identifying the number of gene pools and their degree of connectivity" (2006). Publications, Agencies and Staff of the U.S. Department of Commerce. 463. https://digitalcommons.unl.edu/usdeptcommercepub/463 This Article is brought to you for free and open access by the U.S. Department of Commerce at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications, Agencies and Staff of the U.S. Department of Commerce by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Molecular Ecology (2006) 15, 1419–1439 doi: 10.1111/j.1365-294X.2006.02890.x INVITEDBlackwell Publishing Ltd REVIEW What is a population? An empirical evaluation of some genetic methods for identifying the number of gene pools and their degree of connectivity ROBIN S. WAPLES* and OSCAR GAGGIOTTI† *Northwest Fisheries Science Center, 2725 Montlake Blvd East, Seattle, WA 98112 USA, †Laboratoire d’Ecologie Alpine (LECA), Génomique des Populations et Biodiversité, Université Joseph Fourier, Grenoble, France Abstract We review commonly used population definitions under both the ecological paradigm (which emphasizes demographic cohesion) and the evolutionary paradigm (which emphasizes reproductive cohesion) and find that none are truly operational. -
The Sixth Great Extinction Donations Events "Soon a Millennium Will End
The Rewilding Institute, Dave Foreman, continental conservation Home | Contact | The EcoWild Program | Around the Campfire About Us Fellows The Pleistocene-Holocene Event: Mission Vision The Sixth Great Extinction Donations Events "Soon a millennium will end. With it will pass four billion years of News evolutionary exuberance. Yes, some species will survive, particularly the smaller, tenacious ones living in places far too dry and cold for us to farm or graze. Yet we Resources must face the fact that the Cenozoic, the Age of Mammals which has been in retreat since the catastrophic extinctions of the late Pleistocene is over, and that the Anthropozoic or Catastrophozoic has begun." --Michael Soulè (1996) [Extinction is the gravest conservation problem of our era. Indeed, it is the gravest problem humans face. The following discussion is adapted from Chapters 1, 2, and 4 of Dave Foreman’s Rewilding North America.] Click Here For Full PDF Report... or read report below... Many of our reports are in Adobe Acrobat PDF Format. If you don't already have one, the free Acrobat Reader can be downloaded by clicking this link. The Crisis The most important—and gloomy—scientific discovery of the twentieth century was the extinction crisis. During the 1970s, field biologists grew more and more worried by population drops in thousands of species and by the loss of ecosystems of all kinds around the world. Tropical rainforests were falling to saw and torch. Wetlands were being drained for agriculture. Coral reefs were dying from god knows what. Ocean fish stocks were crashing. Elephants, rhinos, gorillas, tigers, polar bears, and other “charismatic megafauna” were being slaughtered. -
Deme, a Stock, Or a Subspecies? These and Other Definitions
Is It a Deme, a Stock, or a Subspecies? These and Other Definitions BY Robert L. Wilbur Jim Seeb Lisa Seeb and Hal Geiger Regional Information ~e~ort'No. 5598-09 Alaska Department of Fish and Game Commercial Fisheries Management and Development Division Juneau, Alaska March 1998 1 The Regional Information Report Series was established in 1987 to provide an information access system for all unpublished divisional reports. These reports frequently serve diverse ad hoc informational purposes or archive basic uninterpreted data. To accommodate timely reporting of recently collected information, reports in this series undergo only limited internal review and may contain preliminary data; this information may be subsequently finalized and published in the formal literature. Consequently, these reports should not be cited without prior approval of the author or the Division of Commercial Fisheries. INTRODUCTION These population-based definitions were originally prepared in 1996 to aid the Alaska Board of Fisheries in developing consistent applications for the terms used in their guiding principles, and to assist in dialog related to improving management of fish populations. They are archived in this report for reference purposes with only minor changes from the draft originally reviewed by the board 2 years ago. These terms are important because application of the board's guiding principles can affect the management regimes the board selects to achieve its objectives. These decisions will significantly influence the future long-term well-being of fish stocks, as well as the socioeconomic well-being of the resource users. Therefore, it is important the terms be clearly understood for not only their literal meaning, but more importantly, for their pragmatic use in the real world of Alaska's fisheries management. -
Efficient Genetic Markers for Population Biology Paul Sunnucks
REVIEWS Efficient genetic markers for population biology Paul Sunnucks n the past decade, several key Population genetics has come of age. Three laboratory (or, indeed, just to col- advances in molecular genetics important components have come together: laborate with a convenient lab- Ihave greatly increased the im- efficient techniques to examine informative oratory), rather than choosing pact of population genetics on segments of DNA, statistics to analyse DNA the suite of genetic markers that biology. Most important have data and the availability of easy-to-use would best answer the question been: (1) the development of computer packages. Single-locus genetic and then obtaining those data. polymerase chain reaction (PCR), markers and those that produce gene We might consider three levels of which amplifies specified stretches genealogies yield information that is truly molecular change that would pro- of DNA to useable concentrations; comparable among studies. These markers vide information at different lev- (2) the application of evolution- answer biological questions most efficiently els of population biology (Box 1). arily conserved sets of PCR primers and also contribute to much broader First, the most sensitive genetic (e.g. Ref. 1); (3) the advent of investigations of evolutionary, population and signals are genotypic arrays, most hypervariable microsatellite loci2,3; conservation biology. For these reasons, commonly encountered in the and (4) the advent of routine DNA single-locus and genealogical markers should form of multiple microsatellite sequencing in biology laborator- be the focus of the intensive genetic data loci scored in samples of individ- ies. These innovations, coupled collection that has begun owing to the power uals. -
Assessing the Record and Causes of Late Triassic Extinctions
Earth-Science Reviews 65 (2004) 103–139 www.elsevier.com/locate/earscirev Assessing the record and causes of Late Triassic extinctions L.H. Tannera,*, S.G. Lucasb, M.G. Chapmanc a Departments of Geography and Geoscience, Bloomsburg University, Bloomsburg, PA 17815, USA b New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104, USA c Astrogeology Team, U.S. Geological Survey, 2255 N. Gemini Rd., Flagstaff, AZ 86001, USA Abstract Accelerated biotic turnover during the Late Triassic has led to the perception of an end-Triassic mass extinction event, now regarded as one of the ‘‘big five’’ extinctions. Close examination of the fossil record reveals that many groups thought to be affected severely by this event, such as ammonoids, bivalves and conodonts, instead were in decline throughout the Late Triassic, and that other groups were relatively unaffected or subject to only regional effects. Explanations for the biotic turnover have included both gradualistic and catastrophic mechanisms. Regression during the Rhaetian, with consequent habitat loss, is compatible with the disappearance of some marine faunal groups, but may be regional, not global in scale, and cannot explain apparent synchronous decline in the terrestrial realm. Gradual, widespread aridification of the Pangaean supercontinent could explain a decline in terrestrial diversity during the Late Triassic. Although evidence for an impact precisely at the boundary is lacking, the presence of impact structures with Late Triassic ages suggests the possibility of bolide impact-induced environmental degradation prior to the end-Triassic. Widespread eruptions of flood basalts of the Central Atlantic Magmatic Province (CAMP) were synchronous with or slightly postdate the system boundary; emissions of CO2 and SO2 during these eruptions were substantial, but the contradictory evidence for the environmental effects of outgassing of these lavas remains to be resolved. -
Global Catastrophic Risks 2017 INTRODUCTION
Global Catastrophic Risks 2017 INTRODUCTION GLOBAL CHALLENGES ANNUAL REPORT: GCF & THOUGHT LEADERS SHARING WHAT YOU NEED TO KNOW ON GLOBAL CATASTROPHIC RISKS 2017 The views expressed in this report are those of the authors. Their statements are not necessarily endorsed by the affiliated organisations or the Global Challenges Foundation. ANNUAL REPORT TEAM Carin Ism, project leader Elinor Hägg, creative director Julien Leyre, editor in chief Kristina Thyrsson, graphic designer Ben Rhee, lead researcher Erik Johansson, graphic designer Waldemar Ingdahl, researcher Jesper Wallerborg, illustrator Elizabeth Ng, copywriter Dan Hoopert, illustrator CONTRIBUTORS Nobuyasu Abe Maria Ivanova Janos Pasztor Japanese Ambassador and Commissioner, Associate Professor of Global Governance Senior Fellow and Executive Director, C2G2 Japan Atomic Energy Commission; former UN and Director, Center for Governance and Initiative on Geoengineering, Carnegie Council Under-Secretary General for Disarmament Sustainability, University of Massachusetts Affairs Boston; Global Challenges Foundation Anders Sandberg Ambassador Senior Research Fellow, Future of Humanity Anthony Aguirre Institute Co-founder, Future of Life Institute Angela Kane Senior Fellow, Vienna Centre for Disarmament Tim Spahr Mats Andersson and Non-Proliferation; visiting Professor, CEO of NEO Sciences, LLC, former Director Vice chairman, Global Challenges Foundation Sciences Po Paris; former High Representative of the Minor Planetary Center, Harvard- for Disarmament Affairs at the United Nations Smithsonian -
Modeling Population Dynamics
Modeling Population Dynamics Andr´eM. de Roos Modeling Population Dynamics Andr´eM. de Roos Institute for Biodiversity and Ecosystem Dynamics University of Amsterdam Science Park 904, 1098 XH Amsterdam, The Netherlands E-mail: [email protected] December 4, 2019 Contents I Preface and Introduction 1 1 Introduction 3 1.1 Some modeling philosophy . .3 II Unstructured Population Models in Continuous Time 5 2 Modelling population dynamics 7 2.1 Describing a population and its environment . .7 2.1.1 The population or p-state . .7 2.1.2 The individual or i-state . .8 2.1.3 The environmental or E-condition . .9 2.2 Population balance equation . 10 2.3 Characterizing the population . 11 2.4 Population-level and per capita rates . 12 2.5 Model building . 15 2.5.1 Exponential population growth . 15 2.5.2 Logistic population growth . 16 2.5.3 Two-sexes population growth . 17 2.6 Parameters and state variables . 18 2.7 Deterministic and stochastic models . 19 3 Single ordinary differential equations 21 3.1 Explicit solutions . 21 3.2 Numerical integration . 23 3.3 Analyzing flow patterns . 24 3.4 Steady states and their stability . 28 3.5 Units and non-dimensionalization . 32 3.6 Existence and uniqueness of solutions . 35 3.7 Epilogue . 36 4 Competing for resources 37 4.1 Intraspecific competition . 38 i ii CONTENTS 4.1.1 Growth of yeast in a closed container . 38 4.1.2 Bacterial growth in a chemostat . 40 4.1.3 Asymptotic dynamics . 43 4.1.4 Phase-plane methods and graphical analysis . -
Natural Extinctions: Rates and Processes
Extinction: a natural versus human-caused process How do current extinction rates and patterns compare to historical extinctions? The Meaning of Extinct • A species is extinct when no member of the species remains alive anywhere in the world. • A species is extinct in the wild if it is only alive in captivity • A species is locally extinct or extirpated when it is no longer found in an area it used to inhabit but is still found elsewhere • A species is ecologically extinct if it persists in such reduced numbers that its effects on other species is negligible. WHAT ARE BACKGROUND EXTINCTION RATES? • Paleontologists estimate that most species “last” 1-10 million years • If we assume there are 10 million species, 1-10 species go extinct each year (0.00001% to 0.0001% per year) • This rate could be considered a normal background rate against which to gauge mass extinctions THE FIVE MAJOR MASS EXTINCTIONS All genera Well defined genera Generaof Thousands Cretaceous–Tertiary Mass extinction event late Permian- Ordovician–Silurian Devonian Triassic Triassic- Jurassic Millions of years ago CRETACEOUS EXTINCTIONS • 50% of all genera lost, on land and sea • Demise of dinosaurs as dominant group • Impact of extraterrestrial object is the generally accepted cause THE PRESENT • Global biodiversity reached an all time high in the present geological period (about 30,000 years ago) • Biodiversity has declined ever since due to human-induced habitat loss, invasive species, and overexploitation; and is now threatened by pollution, disease, and climate change Our ancestors were hunters & gatherers and not a threat to other species. -
The Palaeoclimatology, Palaeoecology and Palaeoenvironmental Analysis of Mass Extinction Events
Palaeogeography, Palaeoclimatology, Palaeoecology 232 (2006) 190–213 www.elsevier.com/locate/palaeo The palaeoclimatology, palaeoecology and palaeoenvironmental analysis of mass extinction events Richard J. Twitchett School of Earth, Ocean and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK Received 1 December 2004; received in revised form 22 April 2005; accepted 23 May 2005 Abstract Although there is a continuum in magnitude of diversity loss between the smallest and largest biotic crisis, typically most authors refer to the largest five Phanerozoic events as bmass extinctionsQ. In the past 25 years the study of these mass extinction events has increased dramatically, with most focus being on the Cretaceous–Tertiary (K–T) event, although study of the end- Permian event (in terms of research output) is likely to surpass that of the K–T in the next few years. Many aspects of these events are still debated and there is no common cause or single set of climatic or environmental changes common to these five events, although all are associated with evidence for climatic change. The supposed extinction-causing environmental changes resulting from extraterrestrial impact are, at best, equivocal and are unlikely to have been of sufficient intensity or geographic extent to cause global extinction. The environmental consequences of rapid global warming (such as ocean stagnation, reduced upwelling and loss of surface productivity) are considered to have been particularly detrimental to the biosphere in the geological past. The first phase of the Late Ordovician event is clearly linked to rapid global cooling. Palaeoecological studies have demonstrated that feeding mechanism is a key trait that enhances survival chances, with selective detritivores and omnivores usually faring better than suspension feeders or grazers. -
Included & Excluded Disciplines
THESE DISCIPLINES ARE INCLUDED IN THE 2021 CBL COMPETITION DISCIPLINE DIVISION Physical sciences and science technologies ........................................ Physical sciences Astronomy Astrophysics Planetary astronomy and science Astronomy and astrophysics, other Atmospheric sciences and meteorology, general Atmospheric physics and dynamics Meteorology Atmospheric sciences and meteorology, other Chemistry, general Analytical chemistry Inorganic chemistry Organic chemistry Physical chemistry Polymer chemistry Chemical physics Environmental chemistry Theoretical chemistry Chemistry, other Geology/earth science, general Geochemistry Geophysics and seismology Paleontology Hydrology and water resources science Geochemistry and petrology Oceanography, chemical and physical Geological and earth sciences/geosciences, other Physics, general Atomic/molecular physics Elementary particle physics Nuclear physics Optics/optical sciences Condensed matter and materials physics Acoustics Theoretical and mathematical physics Physics, other Materials science Materials chemistry Materials sciences, other Physical sciences, other 2021 INCLUDED DISCIPLINES (CONTINUED) DISCIPLINE DIVISION Mathematics and statistics ......................................................................... Mathematics, general Analysis and functional analysis Topology and foundations Mathematics, other Applied mathematics, general Computational mathematics Computational and applied mathematics Financial mathematics Mathematical biology Applied mathematics, other Statistics, -
Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
life Article Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation Dmitry A. Ruban K.G. Razumovsky Moscow State University of Technologies and Management (the First Cossack University), Zemlyanoy Val Street 73, 109004 Moscow, Russia; [email protected] Received: 2 November 2020; Accepted: 13 November 2020; Published: 14 November 2020 Abstract: Recent eustatic reconstructions allow for reconsidering the relationships between the fifteen Paleozoic–Mesozoic mass extinctions (mid-Cambrian, end-Ordovician, Llandovery/Wenlock, Late Devonian, Devonian/Carboniferous, mid-Carboniferous, end-Guadalupian, end-Permian, two mid-Triassic, end-Triassic, Early Jurassic, Jurassic/Cretaceous, Late Cretaceous, and end-Cretaceous extinctions) and global sea-level changes. The relationships between eustatic rises/falls and period-long eustatic trends are examined. Many eustatic events at the mass extinction intervals were not anomalous. Nonetheless, the majority of the considered mass extinctions coincided with either interruptions or changes in the ongoing eustatic trends. It cannot be excluded that such interruptions and changes could have facilitated or even triggered biodiversity losses in the marine realm. Keywords: biotic crisis; global sea level; life evolution 1. Introduction During the whole Phanerozoic, mass extinctions stressed the marine biota many times. They triggered disappearances of numerous species, genera, families, and even high-order groups of marine organisms, and they were often associated with outstanding environmental catastrophes such as global events of anoxia and euxinia, unusual warming and planetary-scale glaciations, massive volcanism, and extraterrestrial impacts. Mass extinctions were highly complex events, with the intensity amplified by the interplay among atmosphere, oceans, geologic activity, and extraterrestrial influences. The relevant knowledge is huge, and it continues to grow.