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George Mason - BIOL/EVPP - 350
Lecture 4B Light in LakesFreshwaterEcosystemsEVPP/BIOL 350Dr. Kim deMutsertFall 2011Light in Lakes Sun is virtually the only source of energyin natural aquatic habitat; it fuels photosynthesis and heats water Solar constant Rate at which radiat
George Mason - BIOL/EVPP - 350
Lecture 5 Vertical Structure andMixing RegimesEVPP/BIOL 350Freshwater EcosystemsDr. Kim de MutsertFall 2011In freshwater, temperature is themain determinant of density The warmer the water,the better it floats, butice floats even better Water b
George Mason - BIOL/EVPP - 350
BIOL/EVPP 350Freshwater EcosystemsbyDr. Kim de MutsertFall 2011What will you learn in thisclass? Limnology: The Science of InlandWatersThe study of all physical, chemical, andbiological processes in lakes, rivers(streams), and wetlandsWhy is t
George Mason - BIOL/EVPP - 350
EVVP/BIOL 350Lecture 12:Population dynamics and bioticindicesDr Kim de MutsertFall 2011Population dynamicsA population is a group of individuals ofthe same species, living in the same areaPopulation size can be a measure of:- The number of indiv
George Mason - BIOL/EVPP - 350
Lecture 9. Diversity of AquaticOrganisms: Prokaryotes andProtistsEVPP/BIOL 350Dr. Kim de MutsertProkaryotesDistinguished from eukaryotes by theirlack of intracellular organellesGenetic material not enclosed in a nuclearmembrane (there is no nucle
George Mason - BIOL/EVPP - 350
The properties of WaterLecture 4AFreshwater EcosystemsEVPP/BIOL 350Dr. Kim de MutsertWaterThe abundance ofwater is one ofthe most uniqueaspects of PlanetEarth The BluePlanetProperties of Water1.Molecular Structure2.Liquid Nature of Water3
George Mason - BIOL/EVPP - 350
Lecture 20- River andWatershed ManagementFreshwaterEcosystemsEVPP/BIO River Ecology and Management: Lessons from theSource lecture material:Pacific Coastal Ecoregion. 1998. Naiman, R. J. and R. E. Bilby (eds). Springer-EnvironmentalchangeDuring
George Mason - BIOL/EVPP - 350
EVPP/BIOL 350Freshwater EcosystemsLecture 10 Small invertebratesDr. Kim de MutsertFall 2011Zooplankton - CharacteristicsBrachionusPolyarthraKeratella Rotifers Small invertebrates Multicellular,heterotrophic,eukaryotic Suspension feeders Ro
George Mason - BIOL/EVPP - 350
EVPP/BIOL 350FreshwaterEcosystemsLecture 7 StreamChemistryDr. Kim de MutsertFall 2011Stream PhysicochemistrySuspended SedimentsSolutesTemperatureDissolved oxygenSuspended Sediments Suspendedsediment: finegrained solids(between 0.45m and 10
George Mason - BIOL/EVPP - 350
Lecture 3AStreamMorphology andWatershedHydrologyDr. Kim de MutsertEVPP/BIOL 350Freshwater EcosystemsFall 2011Stream Origin While lakes are made byoutside sources, streams make themselves Streams tend to persist; while lakes slowly fill inwith
George Mason - BIOL/EVPP - 350
Lecture 8 WetlandBiogeochemistryEVPP/BIOL 350FreshwaterEcosystemsDr. Kim de MutsertFall 2011Bb Reading:Wetland Biogeochemistry.pp. 177-200 from Wetlands(Mitsch and Gosselink eds.).Wetland Biogeochemistry Wetlands are valuable sources, sinks a
George Mason - BIOL/EVPP - 350
Lecture 3B WetlandCharacteristics:Classificationand HydrologyEVPP/BIOL 350FreshwaterEcosystemshttp:/www.flmnh.ufl.edu/FISH/southflorida/everglades/marshes/marshes.htmlDr. Kim de MutsertFall 2011Wetlands: Regulatory DefinitionWetlands:Those are
George Mason - BIOL/EVPP - 350
Lecture 21 WetlandManagement and RestorationEVPP/BIOL 350Monitoring Watershed RecoveryUntil recovery trends are manifested in someself-sustaining, relatively naturally functioningcondition, restoration or recovery has not trulyoccurredWhen resourc
George Mason - BIOL/EVPP - 350
BIOL/EVPP 350 Freshwater EcosystemsLecture SyllabusFall 2011MW 1:30-2:45 in Research Hall 201Instructors:Dr. Kim de Mutsert, Lecturer and course leader, kdemutse@gmu.eduTerm Assistant Professor, Environmental Science and Policy(703) 993-1043Office
George Mason - GGS - 311
Geographic Information SystemGeographic Information SystemGeographic(GIS)(GIS)(GIS)GIS)What is GIS?Think About GeographyThink About GeographyThinkWhat is Geography? Association of American Geographers definition: Geography is the science of p
George Mason - GGS - 311
Final Examination Study Sheet GGS 311: Introduction to Geographic Information Systems Dr. Matt Rice, Fall 2011 Geographic Data Modeling Longley, chapter 8 GGS-311_-_Lecture6.ppt 1) Definition of a Data Model
George Mason - GGS - 311
GGS 311: Introduction toGeographic InformationSystemsChapter 5: GeoreferencingDr. Matt RiceGeorge Mason UniversityFall 2011IntroductionLongley et al., Chapter 5 Learning Objectives: Learn the requirements for an effective system ofgeoreferencin
George Mason - GGS - 311
Geographic Data ModelingLongley Chapter 8Dr. Matt RiceGeography and GeoinformationScience 311Fall 2011Outline Definitions Data models / modeling GIS data models Topology Example Water facilitiesDefinitions Data model set of constructs for r
George Mason - GGS - 311
Cartography and MapProductionLongley Chapter 12Dr. Matt RiceGeography and Geoinformation Science 311Fall 2011Outline Nature of maps and cartography Principles of map design Composition Symbolization Map series Applications ConclusionsIntrodu
George Mason - GGS - 311
Accuracy & UncertaintyMatt RiceGGS 311 - GMUFall 2011NationalMapPublished byAccuracyUSGSStandardshttp:/egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US%20NationalHorizontalaccuracyFor maps onpublicationNationalMapPublished byAccuracyU
George Mason - GGS - 311
Web GIS / Future of GISDr. Matt RiceGeography and Geoinformation Science311Fall 2011Overview:Future of GISGIS software architectureDataLegal Issues and IPPrivacyPanoramic Map of EurekaCalifornia (l890 1910) availablethrough the Library of Con
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATION SCIENCE 311 INTRODUCTION TO GEOGRAPHIC INFORMATION SYSTEMS Instructor: Dr. Matt Rice Term: Fall 2011 Classroom: Innovation Hall, room 222 Classtime: (GGS 311003: CRN 75396), Tuesday 4:30pm
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATIONSCIENCE 311INTRODUCTION TO GEOGRAPHICINFORMATION SYSTEMSInstructor: Dr. Matt RiceFaculty Office: Research Building I, Room 242Faculty Office Hours: Wednesday, 11:00am-1:00pm or by appointmentEmail: rice@gmu.eduFaculty web
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATIONSCIENCE 311INTRODUCTION TO GEOGRAPHICINFORMATION SYSTEMSInstructor: Dr. Matt RiceFaculty Office: Research Building I, Room 242Faculty Office Hours: Wednesday, 11:00am-1:00pm or by appointmentEmail: rice@gmu.eduFaculty web
George Mason - GGS - 311
GIS Data CollectionLongley, chp. 9Dr. Matt RiceGeorge Mason UniversityFall 2011OverviewIntroductionPrimary data captureSecondary data captureData transferCapturing attribute dataManaging a data capture projectData CollectionOne of most expens
George Mason - GGS - 311
Data Collection TechniquesRasterVectorSecondaryDigitalremotesensingimagesGPSmeasurementsDigitalaerialphotographsPrimarySurveymeasurementsScannedmapsTopographicsurveysDEMsfrommaps ToponymydatasetsfromatlasesPrimary Data CaptureCapture sp
George Mason - GGS - 311
GGS 311 Introduction to GIS Dr. Matt Rice Midterm Exam Study Sheet Fall 2011 1) Read Chapters 1, 7, 5, 3, 9 completely and pay attention to the bold points they are probably going to appear on the exam, p
George Mason - GGS - 311
GGS 311: Introduction to Geographic InformationSystemsChapter 3: RepresentingGeographyDr. Matt RiceGeorge Mason UniversityFall 2011QuestionWhat coordinate system are theseunits likely associated with?621,161 m E3,349,894 m NUTM?PLSS / Townshi
George Mason - GEOL - 102
2/25/11Archean Eonand the Solar System87% of the Earths history is inthe Precambrian!A little background before weget to the Earthmore background All of the planets were formed around thesame time (~4.7bya). They are formed from the same materia
George Mason - GEOL - 102
ArcheanRemember Precambrian time includes 80% of theearth's history, from 4.5 byr - 700 myr. So for the first 500 myr there is nogeologic record. Original crust was thin and composed mainlyof komatite & basalt. Granites have formed from basalts fr
George Mason - GEOL - 102
Cenozoic EventsCenozoic periodEocene and ModernCenozoic Half of the present sea floor was formedsince the end of the Cretaceous! Atlantic and Indian rifting had increased.East CoastFlorida region Erosion is still dominant. Passive margins. Carb
George Mason - GEOL - 102
4/22/11Cenozoic LifeCenozoicEVIDENCE FOR CENOZOICCLIMATE CHANGE Remember in the Cretaceous, climateswere much warmer than today. Although the oceans and atmosphereare affected by the K/T boundary theclimate soon returned to its greenhousestate i
George Mason - GEOL - 102
2/4/11EVOLUTIONLife on EarthTypes of fossilization, againPermineralizationReplacementCarbonizationMolds/casts steinkern Amber Trace fossils Tracks, trails, and burrowsPermineralization Original pore spacesare permeated withgroundwater. Min
George Mason - GEOL - 102
Geologic Time ScalePERIODEPOCHHoloceneNeogeneTertiaryPliocenePaleogenePleistoceneOligoceneMioceneEocenePaleocene0.011.65.323.736.657.8Mesozoic66.4Cretaceous144Jurassic208Triassic245CarboniferousPermianPaleozoicPhanerozoicCen
George Mason - GEOL - 102
Historical GeologyFinal ReviewSpring 2011Current eventsExtinctionKnow 5 largest extinction eventsPermian and Cretaceous extinction eventsMesozoic Tectonics Chapter 13Breakup of PangeaKnow ages of rifting eventsPalisades & Newark formationsDinos
George Mason - GEOL - 102
GeologicTime Scaleagain!Time & GeologyTime v Rock DivisionsEonEraPeriodEpochAgeRock versus TimeEonothemErathemSystemSeriesStageEvolution of geologic time scaleSedgwick and Murchison1Lithology denesComposition of mineral grainsColorTe
George Mason - GEOL - 102
HISTORICAL GEOLOGYGEOLOGY 102, section 002Spring, 2011Instructor: Dr. Stacey Verardosverardo@gmu.edu, 703-993-1045Class hours: Tuesdays and Thursdays 1:30 -2:45pmOffice: David King Hall Room 3037Office Hour: Thursdays, 11am -noonClassroom: Enterpr
George Mason - GEOL - 102
Early ManPrimate groups Prosimmii Tree shrews, lemurs, tarsiers Often nocturnal Anthropoidea Monkeys, apes, humansProsimii & AnthropoideaEarliest primates -Prosimian The earliestrelatives of theprimates werefound in theMesozoic andare simila
George Mason - GEOL - 102
IntroductionTime scaleTime scaleTaxonomicclassicationThis is theversion thatyou will bequizzed on.kingdoms1Factors for fossilization Rapid burial is the best way for successfulfossilization. Most often occur in shallow water with highenergy
George Mason - GEOL - 102
1/18/11HISTORICALGEOLOGYGeology102SowhatisthedierencebetweenGEO101andGEO102? InthisclassyouwilllearnoftheoriginoftheearthandtheevoluJonoftheland,atmosphereandallofitslife. AndthisiswhereyoullneedtolearntheGeologicTimescale. Therewillbeaquizonito
George Mason - GEOL - 102
4/10/11Mesozoic LifeAfter Permian extinction Seas were dominated by an abundance ofmollusks, sea urchins, crustaceans and sh& reptiles. On land, synapsids were replaced byreptiles. crocodiles, turtles, snakes, lizards and dinosaursMesozoicevents
George Mason - GEOL - 102
Mesozoic tectonicsMesozoic era -55-250myrThe breakup of PangaeaRepresents a change tectonically fromcompressional mountain building in theeast and northern parts of the continentto compressional forces on the westernmargin.What was happening ? La
George Mason - GEOL - 102
Rodinia was rifting apartEarly PaleozoicCambrian-SilurianLaurentiaBalticaKazakhstaniaSiberiaChinaGondwana Iapetus Ocean openthen closedRODINIA to PANNOTIANorth America & EuropeCambrianto SilurianDomes and basins1Vendian to OrdovicianCrat
George Mason - GEOL - 102
Late Paleozoic TectonicsLate Paleozoic 410-250 million years ago. Divided into Devonian, Carboniferous,Permian. By the Permian Pangea was assembled. During this time Acadian & Caladonian orogenies Alleghenian & Hercynian orogeniesLatePaleozoicP
George Mason - GEOL - 102
Paleozoic LifeEarly life Fossil record increases with increase infossil hard parts. Vertebrates evolve. Animals move onto land. Vascular plants show up. Also largest mass extinction EVER.Precambrian-Cambrian Invertebrate phylaEarly Cambrian foss
George Mason - GEOL - 102
2/11/11Plate TectonicsJOIDES resolutionP-wavesEARTHQUAKE WAVES P-waves S-waves Surface waves/Long wavesS-waves Oscillate back and forth perpendicular to the directionof wave travel. Change shape of rock. Only in solids. Cause strong movement
George Mason - GEOL - 102
PLEISTOCENE EPOCH1.7myr7 kyr agoExtent of ice during LGMevidenceAn Alps region glaciated valley In 1836 Louis Agassiz, apaleontologist, began to believe thatthe glaciers in the Alps were oncemuch more extensive than today.Glaciated EuropeChanges
George Mason - GEOL - 102
3/3/11Proterozoic2.5bya-540myaProterozoic compared to Archean. Proterozoic has a more modern type ofplate tectonics, sedimentation, and climate. First major Wilson cycle. First large ice age most of Earth cooled. Most BIFs. 42% of Earths history!
George Mason - GEOL - 102
Rocks & MineralsCriteria to be a mineral Occurs naturally as an inorganic solid. Has a specic internal structure. Has a specic chemical composition can exchange occasionally. Has specic physical properties. Minerals can be composed of one element
George Mason - GEOL - 102
Sedimentary ArchivesWhat determines which type ofsedimentary rock forms indifferent environs?Sedimentary EnvironmentsTectonic settingType of rock being weatheredType of transportClimateAmount of pressure & temperatureTimeSedimentary Environment
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam OneSpring 2011Know the TIME SCALEKnow current eventsScience of Historical GeologyChapter 1Scientific MethodUniformitarianismThe 6 KingdomsTaxonomic ClassifiicationsTypes of FossilizationPermineralization
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam TwoCURRENT EVENTSArchean and the Solar System -chapter 8Archean most of Earths History4.6 bya to 700 mya80% of Earths historySolar Nebular HypothesisKnow the planets!Terrestrial & GaseousMeteorites, Astero
George Mason - GEOL - 302
American Mineralogist, Volume 93, pages 16931720, 2008Review PaPeRMineral evolutionRobeRt M. Hazen,1,* DoMinic PaPineau,1 wouteR bleekeR,2 RobeRt t. Downs,3JoHn M. FeRRy,4 tiMotHy J. Mccoy,5 DiMitRi a. sveRJensky,4 anD Hexiong yang3Geophysical Labora
George Mason - GEOL - 306
Thevesoilformingfactors AllinteracttoformthedierenttypesofsoilThevesoilformingfactors Parentalmaterial Canberock Bedrock Residualsoils Transportedmaterialnotinplace TransportedsoilsThevesoilformingfactors LimestonesandstonebasaltThevesoilform
George Mason - GEOL - 306
CATION EXCHANGECAPACITYCLAY MINERALSAnd clay sized fractionThe very very smallveryKaolinite a clay mineral stacks ofhexagonalsheets shownhere are acharacteristicof many clayminerals. Bar is 50m1/1,000,000 m 1/1000 mmhttp:/www.reading.ac.uk
George Mason - GEOL - 306
soilorganicsSpodosolMyakka.TheOcialStateSoilofFloridaAEBhCarbon(cyclelater) dominantlyaddingCtothesoil soweretalkingmoreabouttheupperhorizonAofthesoildominantly.SOMsoilorganicmaFer OrganicmaFerisessenGaltoproducGvesoils improvesphysicala
George Mason - GEOL - 306
MacronutrientsNitrogenxingnodulesh4p:/blog.lib.umn.edu/denis036/thisweekinevoluAon/2007/08/cooperaAon_gets_complex_1.htmlESSENTIALELEMENTS Wearelearningthatsoilsareverycomplexmedium manyreacAonsoccurring thesystemasawholeinaconstantstateofux.Add
George Mason - GEOL - 306
Soil in the newsSome bad- But also some good thingsThe future rests on the soilbeneath our feet.http:/s.ngm.com/2008/09/soil/img/soil-615.jpgPopulation factsPopulationPopulation The world's population will reach 7billion people late this year, a
George Mason - GEOL - 306
SOILORGANICMATTERSOMPeatIsleofLewis,ScotlandSOM EspeciallyinOandA Nutrients Importantfor Supportmicroandmacroorganisms CEC TheyarepartofSOM Holdingwater Tilth. FormaGonofpedsstructure MostofthisnextweekCarboncycle Wewillcoverthisnextweek
George Mason - GEOL - 306
AGoodrichsoilneeds Soil acomplex,breathingen8ty Soil Plants chemistry9macronutrients Neededforplantstogrow C,H,O,N Crucial96%ofaplant K,Ca,Mg,P(phosphorus)S(sulfur)7micoelements Fe,Cl,Mn(Manganese),B(Boron),Cu,Mo(Molybdenum),Zn Lessthan0.010
George Mason - GEOL - 306
SoilPhysicalproper/es.SoilsamplingSoilsampling EarthDay2007 Sunnyside therepresenta5vesoilfortheDistrictofColumbia U.S.Na5onalArboretum.SoilsamplingSoil TextureSoil Texture = %Sand, Silt & Clay in a soil. Soil texture is the single most impor