Fire Mosaics and Habitat Choice in Nomadic Foragers
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Synoptic-Scale Control Over Modern Rainfall and Flood Patterns in the Levant Drylands with Implications for Past Climates
JUNE 2018 ARMONETAL. 1077 Synoptic-Scale Control over Modern Rainfall and Flood Patterns in the Levant Drylands with Implications for Past Climates MOSHE ARMON Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, Jerusalem, Israel ELAD DENTE Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, and Geological Survey of Israel, Jerusalem, Israel JAMES A. SMITH Department of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey YEHOUDA ENZEL AND EFRAT MORIN Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, Jerusalem, Israel (Manuscript received 23 January 2018, in final form 1 May 2018) ABSTRACT Rainfall in the Levant drylands is scarce but can potentially generate high-magnitude flash floods. Rainstorms are caused by distinct synoptic-scale circulation patterns: Mediterranean cyclone (MC), active Red Sea trough (ARST), and subtropical jet stream (STJ) disturbances, also termed tropical plumes (TPs). The unique spatiotemporal char- acteristics of rainstorms and floods for each circulation pattern were identified. Meteorological reanalyses, quantitative precipitation estimates from weather radars, hydrological data, and indicators of geomorphic changes from remote sensing imagery were used to characterize the chain of hydrometeorological processes leading to distinct flood patterns in the region. Significant differences in the hydrometeorology of these three flood-producing synoptic systems were identified: MC storms draw moisture from the Mediterranean and generate moderate rainfall in the northern part of the region. ARST and TP storms transfer large amounts of moisture from the south, which is converted to rainfall in the hyperarid southernmost parts of the Levant. -
Introduction to Theoretical Ecology
Introduction to Theoretical Ecology Natal, 2011 Objectives After this week: The student understands the concept of a biological system in equilibrium and knows that equilibria can be stable or unstable. The student understands the basics of how coupled differential equations can be analyzed graphically, including phase plane analysis and nullclines. The student can analyze the stability of the equilibria of a one-dimensional differential equation model graphically. The student has a basic understanding of what a bifurcation point is. The student can relate alternative stable states to a 1D bifurcation plot (e.g. catastrophe fold). Study material / for further study: This text Scheffer, M. 2009. Critical Transitions in Nature and Society, Princeton University Press, Princeton and Oxford. Scheffer, M. 1998. Ecology of Shallow Lakes. 1 edition. Chapman and Hall, London. Edelstein-Keshet, L. 1988. Mathematical models in biology. 1 edition. McGraw-Hill, Inc., New York. Tentative programme (maybe too tight for the exercises) Monday 9:00-10:30 Introduction Modelling + introduction Forrester diagram + 1D models (stability graphs) 10:30-13:00 GRIND Practical CO2 chamber - Ethiopian Wolf Tuesday 9:00-10:00 Introduction bifurcation (Allee effect) and Phase plane analysis (Lotka-Volterra competition) 10:00-13:00 GRIND Practical Lotka-Volterra competition + Sahara Wednesday 9:00-13:00 GRIND Practical – Sahara (continued) and Algae-zooplankton Thursday 9:00-13:00 GRIND practical – Algae zooplankton spatial heterogeneity Friday 9:00-12:00 GRIND practical- Algae zooplankton fish 12:00-13:00 Practical summary/explanation of results - Wrap up 1 An introduction to models What is a model? The word 'model' is used widely in every-day language. -
Roman Military Operations in Arid Environments (108 BC-AD 400)
Just Deserts: Roman Military Operations in Arid Environments (108 BC-AD 400). Acknowledgements This work would have been impossible without the help, advice and support of a number of people. I am grateful to my mother for her unfailing support and frequent emailed pictures of puppies. I must give great credit to friends Tony Keen, Penny Goodman and Laurie Cubbison for their advice over the process, and their reassurance that much of my reaction to the rigours of the research was both normal and would ease eventually. For academic support I must acknowledge my primary and secondary supervisors Louis Rawlings and Kate Gilliver for their advice and direction, as well as the rest of the academic staff of Cardiff HISAR/SHARE. I owe much to Matthew Kilburn for both the moral support and the discussions of somewhat different asymmetric strategies, as well as Matt Hills for delightful DVD signing queues, Caroline Marks for sanity- saving Saturday coffees, Leslie McMurtry for the art and madness, Tessa Brailsford for the music breaks, and the best guitarist in Physics, Edmund Schluessel. I also gratefully acknowledge my wider online family and my friends who I only get to see in pixels: Erin Chapman, Ray Stillwell, Vicky Pyne, Vicky Hyde, Valerie Kessler, Perri Smith, Lizbet Lewis, Dianne DeSha, Nea Dodson, Celli Lane, Chris Kamnikar, and everyone else on Livejournal or Twitter who have never failed to cheer me when possible and console me when needed. Finally, I wish to thank the indigenous Yemeni and the indigenous Mesoamericans for their discoveries of coffee and chocolate. I couldn't have done it without you. -
Population Genetic Consequences of the Allee Effect and The
Genetics: Early Online, published on July 9, 2014 as 10.1534/genetics.114.167569 Population genetic consequences of the Allee effect and the 2 role of offspring-number variation Meike J. Wittmann, Wilfried Gabriel, Dirk Metzler 4 Ludwig-Maximilians-Universit¨at M¨unchen, Department Biology II 82152 Planegg-Martinsried, Germany 6 Running title: Allee effect and genetic diversity Keywords: family size, founder effect, genetic diversity, introduced species, stochastic modeling 8 Corresponding author: Meike J. Wittmann Present address: Stanford University 10 Department of Biology 385 Serra Mall, Stanford, CA 94305-5020, USA 12 [email protected] 1 Copyright 2014. Abstract 14 A strong demographic Allee effect in which the expected population growth rate is nega- tive below a certain critical population size can cause high extinction probabilities in small 16 introduced populations. But many species are repeatedly introduced to the same location and eventually one population may overcome the Allee effect by chance. With the help of 18 stochastic models, we investigate how much genetic diversity such successful populations har- bor on average and how this depends on offspring-number variation, an important source of 20 stochastic variability in population size. We find that with increasing variability, the Allee effect increasingly promotes genetic diversity in successful populations. Successful Allee-effect 22 populations with highly variable population dynamics escape rapidly from the region of small population sizes and do not linger around the critical population size. Therefore, they are 24 exposed to relatively little genetic drift. It is also conceivable, however, that an Allee effect itself leads to an increase in offspring-number variation. -
Origin of the Sinai-Negev Erg, Egypt and Israel
Quaternary Science Reviews 69 (2013) 28e48 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Origin of the SinaieNegev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R. Muhs a,*, Joel Roskin b, Haim Tsoar b, Gary Skipp a, James R. Budahn a, Amihai Sneh c, Naomi Porat c, Jean-Daniel Stanley d, Itzhak Katra b, Dan G. Blumberg b a U.S. Geological Survey, MS 980, Box 25046, Federal Center, Denver, CO 80225, USA b Dept. of Geography and Environmental Development, Ben-Gurion University of the Negev, P.O.B. 653, Beer-Sheva 84105, Israel c Geological Survey of Israel, 30 Malkhe Israel St., Jerusalem 95501, Israel d Geoarchaeology-Paleobiology Department, E-205 NMNH, MRC-121, Smithsonian Institution, Washington, DC 20013, USA article info abstract Article history: The SinaieNegev erg occupies an area of 13,000 km2 in the deserts of Egypt and Israel. Aeolian sand of Received 22 November 2012 this erg has been proposed to be derived from the Nile Delta, but empirical data supporting this view Received in revised form are lacking. An alternative source sediment is sand from the large Wadi El Arish drainage system in 12 February 2013 central and northern Sinai. Mineralogy of the Negev and Sinai dunes shows that they are high in quartz, Accepted 20 February 2013 with much smaller amounts of K-feldspar and plagioclase. Both Nile Delta sands and Sinai wadi sands, Available online 30 March 2013 upstream of the dunes, also have high amounts of quartz relative to K-feldspar and plagioclase. -
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave http://www.desertusa.com/desert.html In most modern classifications, the deserts of the United States and northern Mexico are grouped into four distinct categories. These distinctions are made on the basis of floristic composition and distribution -- the species of plants growing in a particular desert region. Plant communities, in turn, are determined by the geologic history of a region, the soil and mineral conditions, the elevation and the patterns of precipitation. Three of these deserts -- the Chihuahuan, the Sonoran and the Mojave -- are called "hot deserts," because of their high temperatures during the long summer and because the evolutionary affinities of their plant life are largely with the subtropical plant communities to the south. The Great Basin Desert is called a "cold desert" because it is generally cooler and its dominant plant life is not subtropical in origin. Chihuahuan Desert: A small area of southeastern New Mexico and extreme western Texas, extending south into a vast area of Mexico. Great Basin Desert: The northern three-quarters of Nevada, western and southern Utah, to the southern third of Idaho and the southeastern corner of Oregon. According to some, it also includes small portions of western Colorado and southwestern Wyoming. Bordered on the south by the Mojave and Sonoran Deserts. Mojave Desert: A portion of southern Nevada, extreme southwestern Utah and of eastern California, north of the Sonoran Desert. Sonoran Desert: A relatively small region of extreme south-central California and most of the southern half of Arizona, east to almost the New Mexico line. -
The Corrosive Well Waters of Egypt's Western Desert
The Corrosive Well Waters of Egypt's Western Desert GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1757-O Prepared in cooperation with the Arab Republic of Egypt under the auspices of the United States Agency for International Development The Corrosive Well Waters of Egypt's Western Desert By FRANK E. CLARKE CONTRIBUTIONS TO THE HYDROLOGY OF AFRICA AND THE MEDITERRANEAN REGION GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1757-O Prepared in Cooperation with the Arab Republic of Egypt under the auspices of the United States Agency for International Development UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Clarke, Frank Eldridge, 1913 The corrosive well waters of Egypt's western desert. (Contributions to the hydrology of Africa and the Mediterranean region) (Geological Survey water-supply paper; 1757-0) "Prepared in cooperation with the Arab Republic of Egypt, under the aus pices of the United States Agency for International Development." Bibliography: p. Includes index Supt. of Docs. no. : I 19.16 : 1757-0 1. Corrosion resistant materials. 2. Water, Underground Egypt. 3. Water quality Egypt. 4. Wells Egypt Corrosion. 5. Pumping machinery Cor rosion. I. United States. Agency for International Development. II. Title. III. Series. IV. Series: United States. Geological Survey. Water-supply paper; 1757-0. TA418.75.C58 627'.52 79-607011 For sale by Superintendent of Documents, U.S. Government -
AC28 Inf. 30 (English and Spanish Only / Únicamente En Inglés Y Español / Seulement En Anglais Et Espagnol)
AC28 Inf. 30 (English and Spanish only / únicamente en inglés y español / seulement en anglais et espagnol) CONVENTION ON INTERNATIONAL TRADE IN ENDANGERED SPECIES OF WILD FAUNA AND FLORA ___________________ Twenty-eighth meeting of the Animals Committee Tel Aviv (Israel), 30 August-3 September 2015 REPORT OF THE SECOND MEETING OF THE CFMC/OSPESCA/WECAFC/CRFM WORKING GROUP ON QUEEN CONCH The attached information document has been submitted by the Secretariat on behalf of the FAO Western Central Atlantic Fishery Commission in relation to agenda item 19.* * The geographical designations employed in this document do not imply the expression of any opinion whatsoever on the part of the CITES Secretariat (or the United Nations Environment Programme) concerning the legal status of any country, territory, or area, or concerning the delimitation of its frontiers or boundaries. The responsibility for the contents of the document rests exclusively with its author. AC28 Inf. 30 – p. 1 SLC/FIPS/SLM R1097 FAO Fisheries and Aquaculture Report ISSN 2070-6987 WESTERN CENTRAL ATLANTIC FISHERY COMMISSION Report of the SECOND MEETING OF THE CFMC/OSPESCA/WECAFC/CRFM WORKING GROUP ON QUEEN CONCH Panama City, Panama, 18–20 November 2014 DRAFT Prepared for the 28th meeting of the Animals Committee (A final version in English, French and Spanish is expected to be published by October 2015) 1 PREPARATION OF THIS DOCUMENT This is the report of the second meeting of the Caribbean Fisheries Management Council (CFMC), Organization for the Fisheries and Aquaculture Sector of the Central American Isthmus (OSPESCA), Western Central Atlantic Fishery Commission (WECAFC) and the Caribbean Regional Fisheries Mechanism (CRFM) Working Group on Queen Conch, held in Panama City, Panama, from 18 to 20 November 2014. -
Western Desert, Egypt): Evolution to a Post-Eocene Continental Event
The uppermost deposits of the stratigraphic succession of the Farafra Depression (Western Desert, Egypt): Evolution to a Post-Eocene continental event ⇑ M.E. Sanz-Montero a, , H. Wanas b, M.B. Muñoz-García c,1, L. González-Acebrón c,1, M.V. López d,2 a Dpto. Petrología y Geoquímica, Facultad Ciencias Geológicas, Universidad Complutense de Madrid (UCM), C/José Antonio Novais 12, 28040 Madrid, Spain b Geology Department, Faculty of Science, Menoufia University, Shebin El-Kom, Egypt c Dpto. Estratigrafía, Facultad Ciencias Geológicas, Universidad Complutense de Madrid (UCM), C/José Antonio Novais 12, 28040 Madrid, Spain d Instituto de Geociencias (CSIC, UCM), C/José Antonio Novais 12, 28040 Madrid, Spain Abstract This paper gives insight into continental sedimentary deposits that occur at the uppermost part of the stratigraphic succession present in the north-eastern sector of the Farafra Depression (Western Desert, Egypt). Using space imagery to complete the field work, the geology of the area has been mapped and the presence of a N–S oriented fault system is documented. The analysis of the morphotectonic features related to this fault system allows reconstructing the structural and sedimentological evolution of the area. The study indicates that the continental deposits were accumulated in alluvial systems that uncon-formably overlie shale and evaporitic rocks attributable to the Paleocene–Eocene Esna Formation. The deposits of the Esna Formation show soft-sediment deformation features, which include slump associ- ated to dish and pillar sedimentary structures and provide evidence of syndepositional tectonic activity during the sedimentation of this unit. The outcrops are preserved in two areas on separated fault-bounded blocks. -
Origin of the Sinai-Negev Erg, Egypt and Israel: Mineralogical and Geochemical Evidence for the Importance of the Nile and Sea Level History Daniel R
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- ubP lished Research US Geological Survey 2013 Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R. Muhs U.S. Geological Survey, [email protected] Joel Roskin Ben-Gurion University of the Negev Haim Tsoar Ben-Gurion University of the Negev Gary Skipp U.S. Geological Survey, [email protected] James Budahn U.S. Geological Survey See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Geology Commons, Oceanography and Atmospheric Sciences and Meteorology Commons, Other Earth Sciences Commons, and the Other Environmental Sciences Commons Muhs, Daniel R.; Roskin, Joel; Tsoar, Haim; Skipp, Gary; Budahn, James; Sneh, Amihai; Porat, Naomi; Stanley, Jean-Daniel; Katra, Itzhak; and Blumberg, Dan G., "Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history" (2013). USGS Staff -- Published Research. 931. https://digitalcommons.unl.edu/usgsstaffpub/931 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- ubP lished Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Daniel R. Muhs, Joel Roskin, Haim Tsoar, Gary Skipp, James Budahn, Amihai Sneh, Naomi Porat, Jean-Daniel Stanley, Itzhak Katra, and Dan G. Blumberg This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/usgsstaffpub/931 Quaternary Science Reviews 69 (2013) 28e48 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Origin of the SinaieNegev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R. -
ANDREW M. KRAMER Curriculum Vitae Address
Kramer 1 ANDREW M. KRAMER Curriculum Vitae Address: Department of Integrative Biology University of South Florida 4202 E. Fowler Ave SCA 110 Tampa, FL 33620 (813) 974-2825 email: [email protected] website: http://kramera3.github.io EDUCATION • Ph.D. in Fisheries and Wildlife / Ecology, Evolutionary Biology and Behavior (dual degree), 2007, Michigan State University. Advisor: Orlando Sarnelle • Bachelor of Science, 2000, Saint Louis University, Honors degree, Biology (summa cum laude) ACADEMIC APPOINTMENTS • Assistant Professor, Department of Integrative Biology, University of South Florida, Jan. 2018 – present. • Assistant Research Scientist, Odum School of Ecology, University of Georgia, Aug. 2013 – Dec. 2017. Member of the Graduate Faculty. • Postdoctoral researcher, Odum School of Ecology, University of Georgia, Sept. 2009 – April 2013. Mentor: Dr. John Drake • Instructor, Department of Biology, Gainesville State College, Georgia, Summer 2009. • Postdoctoral researcher, Odum School of Ecology, University of Georgia, Oct. 2007-March 2009. Mentor: Dr. John Drake GRANTS AND AWARDS • Under consideration – National Science Foundation, National Artificial Intelligence Research Institute, “AI Institute: Institute for Advancing Integrative Biology (AIBI)”, 2021-2026. co-PI Kramer, PI: Sudeep Sarkar. ($19,599,253 with $1,959,925 to Kramer). • Under consideration – National Science Foundation, Information Integration and Informatics, “Collaborative Research: Data-Driven modeling of COVID-19 with continuous time Dynamic Mode Decompositions and other approaches”, 2021-2024. co-PI: Kramer, A., PI: J. Rosenfeld. ($859,145 with $340,000 to Kramer). • Under consideration – National Science Foundation, Macrosystems Biology and Neon-enabled Science, “Collaborative Research: MRA: The Paradox of Mosquito Macrosystems: Homogenizing communities and diverging populations in urbanizing landscapes”, 2021-2024. co-PI: Kramer, A., PI: Shannon LaDeau (Cary Institute of Ecosystem Studies). -
The Impact of Fragmented Habitat's Size and Shape on Populations
Math. Model. Nat. Phenom. Vol. 11, No. 4, 2016, pp. 5–15 DOI: 10.1051/mmnp/201611402 The Impact of Fragmented Habitat’s Size and Shape on Populations with Allee Effect W. G. Alharbi, S. V. Petrovskii ∗ Department of Mathematics, University of Leicester, University Road, Leicester LE1 7RH, UK Abstract. This study aims to explore the ways in which population dynamics are affected by the shape and size of fragmented habitats. Habitat fragmentation has become a key concern in ecology over the past 20 years as it is thought to increase the threat of extinction for a number of plant and animal species; particularly those close to the fragment edge. In this study, we consider this issue using mathematical modelling and computer simulations in several domains of various shape and with different strength of the Allee effect. A two-dimensional reaction-diffusion equation (taking the Allee effect into account) is used as a model. Extensive simulations are performed in order to determine how the boundaries impact the population persistence. Our results indicate the following: (i) for domains of simple shape (e.g. rectangle), the effect of the critical patch size (amplified by the Allee effect) is similar to what is observed in 1D space, in particular, the likelihood of population survival is determined by the interplay between the domain size and thee strength of the Allee effect; (ii) in domains of complicated shape, for the population to survive, the domain area needs to be larger than the area of the corresponding rectangle. Hence, it can be concluded that domain size and shape both have crucial effect on population survival.