Chapter One Introduction with Key Findings

Total Page:16

File Type:pdf, Size:1020Kb

Chapter One Introduction with Key Findings CHAPTER ONE INTRODUCTION WITH KEY FINDINGS Dennis D. Murphy ©1999 J.T. Ravizé. All rights reserved. CHAPTER ONE INTRODUCTION WITH KEY FINDINGS Dennis D. Murphy When Mark Twain first spied the immensity This written component of the Lake Tahoe and grandeur of Lake Tahoe he could hardly contain Watershed Assessment is an initial step toward himself, relating in his 1871 travelogue Roughing It: bringing better informed management to the lake “At last the lake burst upon us—a noble and its surrounding basin—to make this era of resto- sheet of blue water lifted six thousand three hundred ration and renewal as successful as possible. The feet above the level of the sea, and walled in by a rim goal is to collect in a single document information of snow-clad mountain peaks that towered aloft full that can be used by land and resource managers to three thousand feet higher still! It was a vast oval, develop a comprehensive conservation plan for the and one would have to use up eighty or a hundred lake and its watershed. Although the lake has been good miles traveling around it. As it lay there with the focus of conservation concern for decades, a the shadows of the mountains brilliantly photo- sense of immediacy now prevails. Scientists warn graphed upon its still surface I thought it must surely that should lake clarity continue to decline at recent be the fairest picture the whole earth affords. rates, Tahoe’s famed aqua waters may be perma- “So singularly clear was the water, that nently compromised in less than a decade. where it was only twenty or thirty feet deep the bot- Not only waters are at risk. The forests of tom was so perfectly distinct that the boat seemed to the Tahoe basin were ravaged by indiscriminate tim- be floating in the air! Yes, where it was even eighty ber harvests more than a century ago and by fire feet deep. Every pebble was distinct, every speckled suppression since then. Today’s landscape is haunted trout, every hand’s-breadth of sand . The water by a ghost of those disruptions to the natural cycle was not merely transparent, but dazzlingly, brilliantly of forest disturbances, differing from its historical so.” structure and composition, subject to devastating Twain’s romance with Lake Tahoe took an insect outbreaks, and at risk of wildfire ignitions as unexpected turn when just hours after he penned never before. So too, many of Tahoe’s meadows and that description a campfire bounded from his con- wetlands have been destroyed and others are in dan- trol, engulfing the surrounding forest and charring ger. Overgrazed at the turn of the century, overde- miles around. veloped since, their unique ecological role in filtering In so many ways Twain’s initial Tahoe ad- sediments from the turbulent stream waters of the venture epitomizes the last century and a half of Tahoe basin and supporting its diverse wildlife has human experience at the lake. The great montane been compromised by any measure. The resident body of water was discovered by excited explorers, species of the lake basin have hardly fared better. rapidly exploited for its diverse natural resources, One of nature’s most productive inland fisheries and then urbanized by waves of settlers. Only in the sustained generations of Native Americans. That past several decades have the effects of our rapa- fishery’s vast uncountable numbers of cutthroat cious appetites for Lake Tahoe’s resources become trout have not just declined, they have vanished. fully evident. And now, after loving and abusing the Nevertheless, yesterday’s environmental Sierra Nevada’s grandest lake for so long, we embark abuse has become today’s environmental challenge, on an era of restoration and renewal. and that challenge is being met at this country’s Lake Tahoe Watershed Assessment 1 Chapter 1 highest levels of government. Recognizing the na- This document, however, does offer explicit rec- tional importance of Lake Tahoe’s diverse resources ommendations for research, monitoring, and an and their dramatic declines, United States Senator adaptive management strategy that will be necessary Harry Reid of Nevada brought President Clinton to inform future management. The task of compiling and Vice President Gore to Lake Tahoe in 1997 for available information for future uses from widely a first-ever presidential forum. There Mr. Clinton dispersed sources has proven to be a fair challenge in affirmed “a shared responsibility to build on our its own right. The watershed assessment science commitments at all levels to be sure the lake and its team has largely restricted itself in this document to environs are protected.” On July 26 of that year the that narrowly defined task. administration promised to fund a diversity of new and expanded efforts directed at water quality, forest Science and the Watershed Assessment management, transportation, and recreation and A list of superlatives has served as the start- tourism, including the development of this water- ing point for most environmental descriptions of shed assessment. Lake Tahoe. The lake is among the most dramatic The watershed assessment thus joins other manifestations of water and geology on earth (Figure ongoing scientific efforts designed to inform policy 1-1). Its depth is more than a third of a mile. Its lake development and resource management at Lake Ta- bottom is hundreds of feet below Carson City, Ne- hoe. Most closely linked to the watershed assessment vada, in the adjacent Great Basin. At nearly two are the water clarity modeling effort being carried hundred square miles, the surface area of the lake out at the University of California at Davis, which is covers nearly two fifths of the Tahoe basin. No intended to advance our understanding of nutrient fewer than 63 small rivers and streams feed Lake and sediment inputs to the lake and their impact on Tahoe, and one large river, the Truckee, drains it its clarity, and the Tahoe Regional Planning Agency’s (Figure 1-2). So much water resides in Tahoe that (TRPA) “real time” management program, which the travel of a snowbank droplet from nearby Mt. attempts to bring reliable information from research Tallac’s alpine summit through the lake and out the and monitoring to resource management in the ba- Truckee River takes seven hundred years. This ex- sin. traordinary residence time of waters in Lake Tahoe is The watershed assessment itself was pro- the driving feature in plans for its restoration. Lake posed in the October 1997 document Presidential Tahoe’s hugeness serves to ameliorate our lesser Forum Deliverables to provide for “the integration of environmental excesses, but that same remarkable ecological knowledge about the Lake Tahoe basin” size creates a long-lasting memory of our worst in- and was “to clearly define the issues and priorities sults. Disturbances to Lake Tahoe from past decades identified during the Presidential visit and to balance will challenge our best management efforts for dec- these priorities in resource management.” The as- ades to come. Nevertheless, fair hope exists for a sessment was further intended to “describe and de- solution to Tahoe’s environmental crisis; more than fine existing conditions, reference variability, and four fifths of the lake’s surrounding basin is in public desired future conditions for key ecosystem elements ownership and can be managed to conserve and en- and environmental indicators.” That job description hance ecosystem health and services (Figure 1-3). was amended; in fact, a mature political process al- The watershed assessment team presup- ready has identified desired future conditions or poses that readers of this document are familiar with “thresholds” for key environmental variables in the the dimensions of the lake, the physical characteris- Lake Tahoe basin, which are evaluated and amended tics of its surrounding landscape, its fate at the hands on a five-year cycle. Appropriately the watershed of settlers from the east, and recent attempts to re- assessment does not prescribe specific management verse more than a century of environmental degen- actions or land use policy. That job correctly resides eration. Those less familiar with Lake Tahoe and its with regional governments, agency staff, and the environment should take advantage of Douglas diverse coalitions of stakeholders at Lake Tahoe. Strong’s wonderful volume Tahoe: from Timber Barons 2 Lake Tahoe Watershed Assessment Chapter 1 Figure 1-1—The Lake Tahoe basin and watershed boundary. Lake Tahoe Watershed Assessment 3 Chapter 1 Figure 1-2—Lake Tahoe tributaries. 4 Lake Tahoe Watershed Assessment Chapter 1 Figure 1-3—Lake Tahoe land ownerships and transportation network. Lake Tahoe Watershed Assessment 5 Chapter 1 to Ecologists(1999). The multivolume Sierra Nevada research reports, articles, and books on the lake and Ecosystem Report, Status of the Sierra Nevada, in- its surrounding watershed dating back to 1878, the cludes a factually dense treatment of Lake Tahoe as a report described information shortfalls that com- case study by Elliott-Fisk et al. (1997) that pairs an promised management of the basin’s air, water, vege- overview of the biophysical challenges faced by ba- tation, fish and wildlife, and resource systems (the sin managers with a description of current institu- latter referring to the cumulative effects of human tional responses to those challenges. These two activities on integrated ecosystem services). More works and the many reports by TRPA that describe than eighty separate research agenda items were pro- its efforts during the past thirty years to meet basin- posed and given “five years as a workable time span wide environmental objectives provide requisite to emphasize current problems over anticipated reading for those desiring to take full value from this ones.” Despite expenditures of more than a million assessment.
Recommended publications
  • Ocean Drilling Program Initial Reports Volume
    Ingle, J. C, Jr., Suyehiro, K., von Breymann, M. T., et al., 1990 Proceedings of the Ocean Drilling Program, Initial Reports, Vol. 128 1. INTRODUCTION, BACKGROUND, AND PRINCIPAL RESULTS OF LEG 128 OF THE OCEAN DRILLING PROGRAM, JAPAN SEA1 Shipboard Scientific Party2 INTRODUCTION in the northern Yamato Basin, first drilled during Leg 127, to conduct two major geophysical experiments aimed at detailing The Japan Sea has been widely viewed as a prime example the structure of the deep crust and upper mantle beneath the of a back-arc basin ever since the emergence of plate tectonic Japan Sea (Fig. 2). We successfully accomplished all of these concepts of convergent margin evolution (Karig, 1971). Abys- tasks. In addition, we cored 190 m into the Miocene volcanic sal water depths exceeding 3000 m point to oceanic crust basement sequence beneath Site 794, initially penetrated beneath the western portions of the sea (Figs. 1 and 2). In during Leg 127, and conducted a pioneering microbiological contrast, tectonically emplaced shallow sills (<150 m) sepa- sampling program at Site 798 to establish the distribution and rate the sea from the adjacent Pacific Ocean and dictate its role of bacteria in the diagenesis of deep marine sediments. unusual oceanographic behavior (Fig. 1). The geology and The new data amassed through Legs 127 and 128 drilling geophysical structure of the Japanese Islands leave no doubt and through geophysical experiments provide heretofore un- regarding the presence of continental crust beneath the Japan available constraints on the timing, rates, and style of forma- Arc, and multiple evidence demonstrates that structurally tion of the deep basins, ridges, and rises of the eastern and isolated continental fragments are present in the Japan Sea central Japan Sea.
    [Show full text]
  • Steinbauer, MJ, Field, R., Grytnes, J
    This is the peer reviewed version of the following article: Steinbauer, M. J., Field, R., Grytnes, J.-A., Trigas, P., Ah-Peng, C., Attorre, F., Birks, H. J. B., Borges, P. A. V., Cardoso, P., Chou, C.-H., De Sanctis, M., de Sequeira, M. M., Duarte, M. C., Elias, R. B., Fernández-Palacios, J. M., Gabriel, R., Gereau, R. E., Gillespie, R. G., Greimler, J., Harter, D. E. V., Huang, T.-J., Irl, S. D. H., Jeanmonod, D., Jentsch, A., Jump, A. S., Kueffer, C., Nogué, S., Otto, R., Price, J., Romeiras, M. M., Strasberg, D., Stuessy, T., Svenning, J.-C., Vetaas, O. R. and Beierkuhnlein, C. (2016), Topography-driven isolation, speciation and a global increase of endemism with elevation. Global Ecol. Biogeogr., 25: 1097– 1107, which has been published in final form at https://doi.org/10.1111/geb.12469. This article may be used for non-commercial purposes in accordance With Wiley Terms and Conditions for self-archiving. Manuscript in press in Global Ecology and Biogeography Topography-driven isolation, speciation and a global increase of endemism with elevation Manuel J. Steinbauer1,2, Richard Field3, John-Arvid Grytnes4, Panayiotis Trigas5, Claudine Ah-Peng6, Fabio Attorre7, H. John B. Birks4,8 Paulo A.V. Borges9, Pedro Cardoso9,10, Chang-Hung Chou11, Michele De Sanctis7, Miguel M. de Sequeira12, Maria C. Duarte13,14, Rui B. Elias9, José María Fernández-Palacios15, Rosalina Gabriel9, Roy E. Gereau16, Rosemary G. Gillespie17, Josef Greimler18, David E.V. Harter1, Tsurng-Juhn Huang11, Severin D.H. Irl1 , Daniel Jeanmonod19, Anke Jentsch20, Alistair S. Jump21, Christoph Kueffer22, Sandra Nogué23,4, Rüdiger Otto15, Jonathan Price24, Maria M.
    [Show full text]
  • Pulsed Miocene Range Growth in Northeastern Tibet: Insights from Xunhua Basin Magnetostratigraphy and Provenance
    Downloaded from gsabulletin.gsapubs.org on July 5, 2012 Pulsed Miocene range growth in northeastern Tibet: Insights from Xunhua Basin magnetostratigraphy and provenance Richard O. Lease1,†, Douglas W. Burbank1, Brian Hough2, Zhicai Wang3, and Daoyang Yuan3 1Department of Earth Science, University of California, Santa Barbara, California 93106, USA 2Department of Earth and Environmental Sciences, University of Rochester, Rochester, New York 14627, USA 3State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China ABSTRACT the north at ca. 22 Ma. Subsequently, growth and deposition initiating in the late Miocene on of the north-trending Jishi Shan occurred both the northern and eastern plateau margins. Sedimentary rocks in Tibetan Plateau at ca. 13 Ma and is highlighted by an accel- Some of the most compelling evidence derives basins archive the spatiotemporal patterns eration in Xunhua Basin accumulation rates from low-temperature thermochronological his- of deformation, erosion, and associated cli- between 12 and 9 Ma, as well as by a signifi - tories in uplifted mountain ranges where age- mate change that resulted from Cenozoic cant change in detrital zircon provenance of depth or time-temperature relationships exhibit a continental collision. Despite growing under- nearby Linxia Basin deposits by 11.5 Ma. Ini- clear transition to rapid cooling. Accelerated late standing of basin development in northeast- tial growth of the WNW-trending Laji Shan Miocene–Pliocene development of the eastern ern Tibet during initial India-Asia collision, in the early Miocene and subsequent growth plateau margin is revealed by detailed thermo- as well as in the late Miocene–Holocene, sur- of the north-trending Jishi Shan ~10 m.y.
    [Show full text]
  • Beyond Refugia: New Insights on Quaternary Climate Variation and the Evolution of Biotic Diversity in Tropical South America
    Beyond Refugia: New insights on Quaternary climate variation and the evolution of biotic diversity in tropical South America Paul A. Baker1*, Sherilyn C. Fritz2*, David S. Battisti3, Christopher W. Dick4, Oscar M. Vargas4, Gregory P. Asner5, Roberta E. Martin5, Alexander Wheatley1, Ivan Prates6 1 Division of Earth and Ocean Sciences, Duke University, Durham, NC 27708, USA, [email protected] 2 Department of Earth and Atmospheric Sciences and School of Biological Sciences, University of Nebraska-Lincoln, Lincoln, NE 68588, USA, [email protected] 3 Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195, USA 4 Department of Ecology & Evolutionary Biology, University of Michigan, Ann Arbor, MI 48109, USA 5 Center for Global Discovery and Conservation Science, Arizona State University, Tucson, AZ 85287, USA 6 Department of Vertebrate Zoology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA * These authors contributed equally to this work. Abstract Haffer’s (1969) Pleistocene refuge theory has provided motivation for 50 years of investigation into the connections between climate, biome dynamics, and neotropical speciation, although aspects of the original theory are not supported by subsequent studies. Recent advances in paleoclimatology suggest the need for reevaluating the role of Quaternary climate on evolutionary history in tropical South America. In addition to the many repeated large-amplitude climate changes associated with Pleistocene glacial-interglacial stages (~ 40 kyr and 100 kyr cyclicity), we highlight two aspects of Quaternary climate change in tropical South America: (1) an east-west precipitation dipole, induced by solar radiation changes associated with Earth’s precessional variations (~20 kyr cyclicity); and (2) periods of anomalously high precipitation that persisted for centuries-to-millennia (return frequencies ~1500 yr) congruent with cold “Heinrich events” and cold Dansgaard-Oeschger “stadials” of the North Atlantic region.
    [Show full text]
  • Carya Eral Roots
    VIEWPOINT HORTSCIENCE 51(6):653–663. 2016. nut (seed) has hypogeal germination and forms a dominate taproot with abundant lat- Carya eral roots. Leaves are odd-pinnately com- Crop Vulnerability: pound with 11–17 leaflets, borne in alternate L.J. Grauke1 arrangement, with reduction in leaflet number, size, and pubescence as the tree matures. USDA–ARS Pecan Breeding and Genetics, 10200 FM 50, Somerville, TX Seedlings have long juvenility (5–12 years) 77879 and bear imperfect flowers at different loca- tions on the tree. Male and female flowers Bruce W. Wood mature at different times (dichogamy). Male USDA–ARS Southeastern Fruit and Tree Nut Research Laboratory, 21 flowers are borne on staminate catkins in Dunbar Road, Byron, GA 31008 fascicles of three, with catkin groups formed on opposite sides of each vegetative bud, Marvin K. Harris sometimes with a second pair above, borne Department of Entomology (Professor Emeritus), Texas A&M University, opposite each other, at 90° to the first. The College Station, TX 77843 catkins are borne at the base of the current season’s growth or from more distal buds of Additional index words. Carya illinoinensis, germplasm, diversity, breeding, repository, the previous season whose vegetative axis characterization aborts after pollen shed. This pattern of catkin formation is characteristic of all members of Abstract. Long-established native tree populations reflect local adaptations. Represen- section Apocarya, but is distinct from the other tation of diverse populations in accessible ex situ collections that link information on sections of the genus (Figs. 2–4). Pollen is phenotypic expression to information on spatial and temporal origination is the most produced in very large quantities and is carried efficient means of preserving and exploring genetic diversity, which is the foundation of by wind.
    [Show full text]
  • Distance Dispersal Or Postglacial Contraction?
    Received: 5 June 2017 | Revised: 13 November 2017 | Accepted: 20 November 2017 DOI: 10.1002/ece3.3719 ORIGINAL RESEARCH Long- distance dispersal or postglacial contraction? Insights into disjunction between Himalaya–Hengduan Mountains and Taiwan in a cold- adapted herbaceous genus, Triplostegia Yan-Ting Niu1,2 | Jian-Fei Ye1,2,3 | Jin-Long Zhang4 | Ji-Zhong Wan5 | Tuo Yang1 | Xiao-Xin Wei1 | Li-Min Lu1,6 | Jian-Hua Li7 | Zhi-Duan Chen1 1State Key Laboratory of Systematic and Evolutionary Botany, Institute of Abstract Botany, Chinese Academy of Sciences, Beijing, Current disjunct patterns can result from long- distance dispersal or postglacial con- China traction. We herein investigate the evolutionary history of Triplostegia to elucidate the 2University of Chinese Academy of Sciences, Beijing, China disjunction between the Himalaya–Hengduan Mountain region (HHM) and Taiwan 3Beijing Botanical Garden, Institute of (TW). Genetic structure of Triplostegia was investigated for 48 populations using se- Botany, Chinese Academy of Sciences, Beijing, quences from five chloroplast loci and the ribosomal nuclear internal transcribed China 4Flora Conservation Department, Kadoorie spacer. Divergence time estimation, ancestral area reconstruction, and species distri- Farm and Botanic Garden, Hong Kong SAR, bution modeling (SDM) were employed to examine the biogeographic history of China Triplostegia. Substantial genetic differentiation among populations from southwestern 5School of Nature Conservation, Beijing Forestry University, Beijing, China China (SW), Central China (CC), and TW was detected. Triplostegia was inferred to 6Sino-African Joint Research Center, Chinese have originated in SW, and diversification began during the late Miocene; CC was Academy of Sciences, Wuhan, China colonized in the mid- Pliocene, and TW was finally colonized in the early Pleistocene.
    [Show full text]
  • Bebras Australia Computational Thinking Challenge
    Bebras Australia Computational Thinking Challenge 2021 Solutions Guide Round 1 Primary School Grades 3-6 bebras.edu.au Bebras Australia Computational Thinking Challenge Bebras is an international initiative aiming The Bebras international community has to promote Computational Thinking skills now grown to 60 countries with over 2.9 among students. million students participating worldwide! Started in 2004 by Professor Valentina Bebras Australia began in 2014 and is now Dagiene from the University of Vilnius, administered through CSIRO Digital Careers. ‘Bebras’ is Lithuanian for beaver. This refers to their collaborative nature and strong In Australia, the Bebras Challenge takes work ethic. place in March and August-September each year. As of 2020, two separate challenges are The International Bebras Committee meets offered for each round. annually to assess potential questions and share resources. Questions are submitted To find out more and register for the by member countries and undergo a vetting next challenge, visit bebras.edu.au process. Engaging young 523 minds for Australian schools participated in Australia’s Bebras R1 2021 digital future 32 311 Australian students participated in CSIRO Digital Careers supports teachers and encourages Bebras R1 2021 students’ understanding of digital technologies and the foundational skills they require in an ever-changing 2.9 million workforce. Growing demand for digital skills isn’t just students participate limited to the ICT sector. All jobs of the future will require worldwide them, from marketing and multimedia through to agriculture, finance and health. Digital Careers prepares students with the knowledge and skills they need to thrive in the workforce of tomorrow.
    [Show full text]
  • NOAA Atlas 14 Vol 7
    NOAA Atlas 14 Precipitation-Frequency Atlas of the United States Volume 7 Version 2.0: Alaska Sanja Perica1, Douglas Kane2, Sarah Dietz1, Kazungu Maitaria1, Deborah Martin1, Sandra Pavlovic1, Ishani Roy1, Svetlana Stuefer2, Amy Tidwell2, Carl Trypaluk1, Dale Unruh1, Michael Yekta1, Erica Betts2, Geoffrey Bonnin1, Sarah Heim1, Lillian Hiner1, Elizabeth Lilly2, Jayashree Narayanan2, Fenglin Yan1, Tan Zhao1 1U.S. Department of Commerce, National Oceanic and Atmospheric Administration, National Weather Service and 2University of Alaska Fairbanks, Water and Environmental Research Center Silver Spring, Maryland, 2012 NOAA Atlas 14 Precipitation-Frequency Atlas of the United States Volume 7 Version 2.0: Alaska Sanja Perica1, Douglas Kane2, Sarah Dietz1, Kazungu Maitaria1, Deborah Martin1, Sandra Pavlovic1, Ishani Roy1, Svetlana Stuefer2, Amy Tidwell2,Carl Trypaluk1,Dale Unruh1,Michael Yekta1, Erica Betts2, Geoffrey Bonnin1, Sarah Heim1, Lillian Hiner1, Elizabeth Lilly2, Jayashree Narayanan2, Fenglin Yan1, Tan Zhao1 1U.S. Department of Commerce, National Oceanic and Atmospheric Administration, National Weather Service and 2University of Alaska Fairbanks, Water and Environmental Research Center Silver Spring, Maryland, 2012 Library of Congress Classification Number G1046 .C8 U6 no.14 v.7 (2012) Table of Contents 1. Abstract ............................................................................................................................ 1 2. Preface to Volume 7 .........................................................................................................
    [Show full text]
  • The Variable Lifespan of the Laramide Orogeny
    Location, location, location: The variable lifespan of the Laramide orogeny Peter Copeland1, Claire A. Currie2, Timothy F. Lawton3, and Michael A. Murphy1 1Department of Earth and Atmospheric Sciences, University of Houston, Houston, Texas 77204, USA 2Department of Physics, University of Alberta, Edmonton, Alberta T6G 2E1, Canada, 3Centro de Geociencias, Universidad Nacional Autónoma de México, Querétaro 76230, México ABSTRACT our boundary passes through the northwest edge The Laramide orogeny had a spatially variable lifespan, which we explain using a geody- of the classic Laramide province (DeCelles, namic model that incorporates onset and demise of flat-slab subduction. Laramide shortening 2004), we designate this line as the northwest and attendant uplift began in southeast California (USA) at ca. 90 Ma, swept to the northeast to margin of the region we consider below. arrive in the Black Hills of South Dakota (USA) at ca. 60 Ma, and concluded in South Dakota Figure 1B shows the age of the various phe- within ~10 m.y. During subsequent slab rollback, the areal extent of Laramide deformation nomena listed above versus distance along a decreased as the eastern edge of active deformation retreated to the southwest rapidly from line of projection, A-A′ (Fig. 1A), which has a ca. 55 to 45 Ma and more slowly from ca. 45 to 40 Ma, with deformation ultimately ceasing bearing of 045 and passes through the middle of in the southwestern part of the orogen at ca. 30 Ma. Geodynamic modeling of this process the classic Laramide province (DeCelles, 2004). suggests that changes in the strength of the North America plate and densification of the Far- This approach compresses the spatial complex- allon plate played important roles in controlling the areal extent of the Laramide orogen and ity of a continent-scale orogen onto a single line hence the lifespan of the orogenic event at any particular location in western North America.
    [Show full text]
  • Madden & Cook Proposal
    NSF PROPOSAL--DRAFT Summary This proposal suggests integrating two independent methods of studying South America's climate history, namely, numerical models and the fossil record. We propose running an atmospheric general circulation model (AGCM) with various scenarios of paleo-topography and sea surface temperatures (SSTs) to mimic the general climate history of South America from the Miocene to the present. These global model integrations will provide distributions of precipitation, temperature, and other biotically significant climate variables for South America. Using these global GCM boundary conditions, we will embed more detailed regional or mesoscale topographic histories for four areas; the northern Andes of Colombia & Ecuador, the Bolivian altiplano, western and northwestern Argentina, and Patagonia. The climatologies of these four embedding experiments will summarize patterns of regional climate change resulting from Neogene tectonism and uplift at a scale more comensurate with the geographic and temporal resolution of the fossil record. Then, arguing from the correlation between climate, primary productivity and species richness patterns in living mammals, we will compare the biotic implications of the embedded regional climate scenarios with the best available sequences of the Neogene fossil mammal record in South America. We will integrate the GCM output with data on primary productivity, plant and mammal species richness using Geographic Information System (GIS) cartographic control which will serve as the basis for 1) matching geographic and temporal resolution between the GCM, primary productivity, and species richness datasets, 2) statistical tests of geographic goodness of fit, and 3) as the mapped basis for regional mesoscale predictions about species richness patterns in the fossil record.
    [Show full text]
  • 39. Seismic Stratigraphy of the Neogene Sequence at Site 5871
    39. SEISMIC STRATIGRAPHY OF THE NEOGENE SEQUENCE AT SITE 5871 Alain Mignot and Alain Mauffret, Département de Géologie Dynamique, Université Pierre et Marie Curie2 INTRODUCTION ing and canyon erosion are the main sedimentary pro- cesses acting at present (Fig. 4, location A). Interbedded The Lord Howe Rise terminates northward against strong reflections (Fig. 4, location B), however, make the the southeast-trending Fairway Ridge. The Fairway Ba- section appear similar to the basal sequence of the Rhone sin lies to the south of this juncture between the Fairway deep-sea fan (Droz, 1982) and indicate intermittent de- Ridge and the Lord Howe Rise. Eastward off the Fair- position. In this area the deposits are rare and unstable. way Ridge lies the New Caledonia Basin. Lansdowne Downslope, a fan is formed by the coalescing of sedi- Bank, a 137-km-long, 50-km-wide fossil atoll, lies on mentary wedges deposited at the mouths of several can- the northern termination of the Lord Howe Rise at the yons. The main channel of the fan is bounded by asym- juncture with the Fairway Ridge (Fig. 1). metrical levees (Fig. 5, locations A and B). Discontinu- These local submarine ridges are isolated from terrig- ous reflections within the channel levees indicate an enous input from Australia to the west and New Caledo- environment of deposition in which presumed fine- nia to the east. Consequently, they are mantled by undi- grained sediments settle out of turbidity currents while luted Neogene pelagic sedimentation that records Neo- the main channel continues to be the locus of transport gene paleooceanography.
    [Show full text]
  • Understanding Broad-Scale Vegetation Patterns Abst
    58th Annual Symposium of the International Association for Vegetation Science: IAVS Symposium, Brno 2015 – Abstracts th Understanding broad-scale 58 vegetation patterns 19 – 24 July 2015, Brno, Czech Republic Abstracts www.iavs2015.cz 58th Annual Symposium of the International Association for Vegetation Science Abstracts 58th Annual Symposium of the International Association for Vegetation Science: Understanding broad-scale vegetation patterns 19 – 24 July 2015, Brno, Czech Republic Abstracts Edited by Milan Chytrý, David Zelený & Eva Hettenbergerová Masaryk University, Brno, 2015 Local Organizing Committee Milan Chytrý Michal Hájek Radim Hédl Tomáš Herben Eva Hettenbergerová Soňa Hroudová Jan Lepš Zdeňka Lososová Jan Roleček Lubomír Tichý David Zelený IAVS Advisory Committee Martin Diekmann (Germany) – IAVS President Robert K. Peet (USA) – IAVS Vice President and Chair of the Publications Committee Michael Palmer (USA) – IAVS Vice President and Chair of the Membership Committee Javier Loidi (Spain) – IAVS Vice President and Chair of the Meetings Committee Alicia Acosta (Italy) – IAVS Vice President Valério Pillar (Brazil) – IAVS Vice President Susan Wiser (New Zealand) – IAVS Secretary Stefan Bradham (USA) – IAVS Administrator Meelis Pärtel (Estonia) – Chair of the Chief Editors of the IAVS Journals Alessandra Fidelis (Brazil) – Chair of the IAVS Global Sponsorship Committee Joop H.J. Schaminée (The Netherlands) – Chair of the IAVS Awards Committee Kerry Woods (USA) – Chair of the IAVS Ethics Committee Ladislav Mucina (Australia) – Organizer
    [Show full text]