Source: Natureserve, US GAP, Landfire Mapping Approach: Inductive Modeling

Total Page:16

File Type:pdf, Size:1020Kb

Source: Natureserve, US GAP, Landfire Mapping Approach: Inductive Modeling 95°W 90°W 85°W Actual Terrestrial Ecosystems in the Gulf Coast Region Source: NatureServe, US GAP, LandFire Mapping Approach: Inductive Modeling 30°N 30°N Scale - 1:1,000,000 0 50 100 200 Miles 0 50 100 200 Kilometers Terrestrial Ecosystems Non-Specific Disturbed East-Central Texas Plains Riparian Forest Southern Coastal Plain Blackland Prairie and Woodland West Gulf Coastal Plain Pine-Hardwood Flatwoods Central Florida Wet Prairie and Herbaceous Seep Open Water East-Central Texas Plains Floodplain Forest Southwest Florida Dune and Coastal Grassland Atlantic Coastal Plain Clay-Based Carolina Bay Wetland Florida Big Bend Salt and Brackish Tidal Marsh Developed Atlantic Coastal Plain Fall-line Sandhills Longleaf Pine Woodland Texas-Louisiana Coastal Prairie Southern Coastal Plain Nonriverine Cypress Dome Florida Big Bend Fresh and Oligohaline Tidal Marsh Quarries/Strip Mines/Gravel Pits Atlantic Coastal Plain Upland Longleaf Pine Woodland East Gulf Coastal Plain Dune and Coastal Grassland Southern Coastal Plain Seepage Swamp and Baygall South Florida Mangrove Swamp Agriculture - Pasture/Hay West Gulf Coastal Plain Upland Longleaf Pine Forest and Woodland Central and Upper Texas Coast Dune and Coastal Grassland West Gulf Coastal Plain Seepage Swamp and Baygall Southern Atlantic Coastal Plain Depression Pondshore Agriculture - Cultivated Crops and Irrigated Agriculture East Gulf Coastal Plain Interior Upland Longleaf Pine Woodland Tamaulipan Savanna Grassland East Gulf Coastal Plain Tidal Wooded Swamp Central Atlantic Coastal Plain Nonriverine Swamp & Wet Hardwood Forest Upper Texas Coast Beach Florida Longleaf Pine Sandhill South Texas Lomas Tamaulipan Floodplain West Gulf Coastal Plain Near-Coast Large River Swamp Louisiana Beach Southern Coastal Plain Mesic Slope Forest Tamaulipan Clay Grassland Tamaulipan Arroyo Shrubland Atlantic Coastal Plain Small Brownwater River Floodplain Forest Southeast Florida Beach East-Central Texas Plains Pine Forest and Woodland South Texas Sand Sheet Grassland Mississippi River Riparian Forest South Florida Bayhead Swamp South Florida Shell Hash Beach South Florida Pine Rockland South Texas Dune and Coastal Grassland Mississippi River Low Floodplain (Bottomland) Forest Atlantic Coastal Plain Small Blackwater River Floodplain Forest Florida Panhandle Beach Southern Coastal Plain Oak Dome and Hammock Successional Shrub/Scrub Lower Mississippi River Flatwoods Red River Large Floodplain Forest Southwest Florida Beach West Gulf Coastal Plain Pine-Hardwood Forest Atlantic Coastal Plain Fall-line Sandhills Longleaf Pine Woodland Southern Coastal Plain Hydric Hammock Atlantic Coastal Plain Blackwater Stream Floodplain Forest Texas Coastal Bend Beach East Gulf Coastal Plain Interior Shortleaf Pine-Oak Forest Introduced Wetland Vegetation - Treed West Gulf Coastal Plain Small Stream and River Forest Southern Coastal Plain Nonriverine Basin Swamp Southern Appalachian Oak Forest West Gulf Coastal Plain Sandhill Oak & Shortleaf Pine Forest & Woodland Clearcut - Grassland/Herbaceous West Gulf Coastal Plain Large River Floodplain Forest East Gulf Coastal Plain Small Stream and River Floodplain Forest West Gulf Coastal Plain Mesic Hardwood Forest East Gulf Coastal Plain Maritime Forest Successional Shrub/Scrub (Clear Cut) East Gulf Coastal Plain Large River Floodplain Forest Southern Coastal Plain Blackwater River Floodplain Forest East Gulf Coastal Plain Northern Mesic Hardwood Slope Forest Lower Mississippi River Dune Woodland and Forest Recently Burned Forbland South Florida Everglades Sawgrass Marsh Texas-Louisiana Coastal Prairie Slough Southern Coastal Plain Limestone Forest Mississippi Delta Maritime Forest Managed Tree Plantation South Florida Wet Marl Prairie West Gulf Coastal Plain Nonriverine Wet Hardwood Flatwoods East Gulf Coastal Plain Southern Loess Bluff Forest Florida Peninsula Inland Scrub Modified/Managed Southern Tall Grassland East Gulf Coastal Plain Savanna and Wet Prairie Mississippi River Bottomland Depression Southern Coastal Plain Dry Upland Hardwood Forest Atlantic Coastal Plain Xeric River Dune South Florida Dwarf Cypress Savanna Texas Saline Coastal Prairie North-Central Interior Rich Swamp South Florida Hardwood Hammock Tamaulipan Mixed Deciduous Thornscrub South Florida Pine Flatwoods Floridian Highlands Freshwater Marsh Southern Coastal Plain Herbaceous Seep and Bog Atlantic Coastal Plain Dry and Dry-Mesic Oak Forest Tamaulipan Mesquite Upland Scrub South Florida Cypress Dome Western Great Plains Depressional Wetland Systems South Florida Slough, Gator Hole, and Willow Head Southwest Florida Coastal Strand and Maritime Hammock Tamaulipan Calcareous Thornscrub Southern Atlantic Coastal Plain Wet Pine Savanna & Flatwoods Gulf Coastal Plain Tidal Marshes Central Atlantic Coastal Plain Fresh and Oligohaline Tidal Marsh 25°N Southeast Florida Coastal Strand and Maritime Hammock West Gulf Coastal Plain Catahoula Barrens West Gulf Coastal Plain Wet Longleaf Pine Savanna & Flatwoods Central Atlantic Coastal Plain Salt and Brackish Tidal Marsh Mississippi River Floodplain and Riparian Forest Central and South Texas Coastal Fringe Forest and Woodland Great Lakes Wet-Mesic Lakeplain Prairie Atlantic Coastal Plain Peatland Pocosin and Canebrake Atlantic Coastal Plain Indian River Lagoon Tidal Marsh 25°N West Gulf Coastal Plain Chenier/Upper Texas Coastal Fringe Forest & Woodland Southern Blackland Tallgrass Prairie Central Florida Pine Flatwoods Southeastern Coastal Plain Interdunal Wetland Atlantic Coastal Plain Mesic Hardwood Forest Florida Dry Prairie East Gulf Coastal Plain Near-Coast Pine Flatwoods Mississippi Sound Salt and Brackish Tidal Marsh East-Central Texas Plains Post Oak Savanna and Woodland West Gulf Coastal Plain Southern Calcareous Prairie South-Central Interior / Upper Coastal Plain Wet Flatwoods Central Florida Herbaceous Pondshore Projection: Universal Transverse Mercator, Datum NAD83 95°W 90°W 85°W.
Recommended publications
  • Ghosts of the Western Glades Just Northwest of Everglades National Park Lies Probably the Wildest, Least Disturbed Natural Area in All of Florida
    Discovering the Ghosts of the Western Glades Just Northwest of Everglades National Park lies probably the wildest, least disturbed natural area in all of Florida. Referred to as the Western Everglades (or Western Glades), it includes Fakahatchee Strand State Preserve and Big Cypress National Preserve. Environmentalists that pushed for the creation of Everglades National Park originally wanted this area included in it. But politics and lack of funds prevented this. Several decades passed before Big Cypress National Preserve was born in 1974. Preserves have slightly less restrictive rules than national parks. So how is the Big Cypress Swamp distinct from the Everglades? Even though both habitats have many similarities (sawgrass prairies & tree islands, for instance), the Big Cypress Swamp is generally 1-2 feet higher in elevation. Also, it has a mainly southwesterly flow of water, dumping into the “ten thousand islands” area on Florida’s Gulf of Mexico coast and serving as an important watershed for the River of Grass to the south. Then, of course, there are the cypress trees. Cypress Trees Not surprisingly, of course, is the fact that the Big Cypress Swamp has about 1/3 of its area covered in cypress trees. Mostly they are the small “dwarf pond cypress” trees. (“Big” refers to the large mass of land not the size of the trees.) A few locations, however, still do boast the impressive towering “bald cypress” trees but most of those were logged out between the years 1913 - 1948. Ridge & Slough Topography Topography simply means the relief (or elevation variances) of any particular area of land.
    [Show full text]
  • Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
    58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region.
    [Show full text]
  • Southeastern Coastal Plains-Caribbean Region Report
    Southeastern Coastal Plains-Caribbean Region Report U.S. Shorebird Conservation Plan April 10, 2000 (Revised September 30, 2002) Written by: William C. (Chuck) Hunter U.S. Fish and Wildlife Service 1875 Century Boulevard Atlanta, Georgia 30345 404/679-7130 (FAX 7285) [email protected] along with Jaime Collazo, North Carolina State University, Raleigh, NC Bob Noffsinger, U.S. Fish and Wildlife Service, Manteo, NC Brad Winn, Georgia DNR Wildlife Resources Division, Brunswick, GA David Allen, North Carolina Wildlife Resources Commission, Trenton, NC Brian Harrington, Manomet Center for Conservation Sciences, Manomet, MA Marc Epstein, U.S. Fish and Wildlife Service, Merritt Island NWR, FL Jorge Saliva, U.S. Fish and Wildlife Service, Boqueron, PR Executive Summary This report articulates what is needed in the Southeastern Coastal Plains and Caribbean Region to advance shorebird conservation. A separate Caribbean Shorebird Plan is under development and will be based in part on principles outlined in this plan. We identify priority species, outline potential and present threats to shorebirds and their habitats, report gaps in knowledge relevant to shorebird conservation, and make recommendations for addressing identified problems. This document should serve as a template for a regional strategic management plan, with step-down objectives, local allocations and priority needs outlined. The Southeastern Coastal Plains and Caribbean region is important for breeding shorebirds as well as for supporting transient species during both northbound
    [Show full text]
  • Limpkin Aramus Guarauna Taxa: Avian SE-GAP Spp Code: Blimp Order: Gruiformes ITIS Species Code: 176197 Family: Aramidae Natureserve Element Code: ABNMJ01010
    Limpkin Aramus guarauna Taxa: Avian SE-GAP Spp Code: bLIMP Order: Gruiformes ITIS Species Code: 176197 Family: Aramidae NatureServe Element Code: ABNMJ01010 KNOWN RANGE: PREDICTED HABITAT: P:\Proj1\SEGap P:\Proj1\SEGap Range Map Link: http://www.basic.ncsu.edu/segap/datazip/maps/SE_Range_bLIMP.pdf Predicted Habitat Map Link: http://www.basic.ncsu.edu/segap/datazip/maps/SE_Dist_bLIMP.pdf GAP Online Tool Link: http://www.gapserve.ncsu.edu/segap/segap/index2.php?species=bLIMP Data Download: http://www.basic.ncsu.edu/segap/datazip/region/vert/bLIMP_se00.zip PROTECTION STATUS: Reported on March 14, 2011 Federal Status: --- State Status: FL (SSC) NS Global Rank: G5 NS State Rank: AL (SNA), FL (S3), GA (S1S2), IL (SNA), MD (SNA), MS (SNA), NC (SNA), TX (SNA), VA (SNA), NS (SNA) bLIMP Page 1 of 4 SUMMARY OF PREDICTED HABITAT BY MANAGMENT AND GAP PROTECTION STATUS: US FWS US Forest Service Tenn. Valley Author. US DOD/ACOE ha % ha % ha % ha % Status 1 34,779.2 < 1 120.6 < 1 0.0 0 0.0 0 Status 2 18,984.4 < 1 26,563.7 < 1 0.0 0 0.0 0 Status 3 0.0 0 154,688.7 2 0.0 0 31,698.2 < 1 Status 4 0.0 0 0.0 0 0.0 0 0.0 0 Total 53,763.7 < 1 181,373.0 3 0.0 0 31,698.2 < 1 US Dept. of Energy US Nat. Park Service NOAA Other Federal Lands ha % ha % ha % ha % Status 1 0.0 0 362,645.8 5 0.0 0 8,464.4 < 1 Status 2 0.0 0 3,173.0 < 1 12,062.5 < 1 77.1 < 1 Status 3 0.0 0 270,295.1 4 0.0 0 0.0 0 Status 4 0.0 0 0.0 0 0.0 0 0.0 0 Total 0.0 0 636,113.9 9 12,062.5 < 1 8,541.5 < 1 Native Am.
    [Show full text]
  • Evaluating the Functional Response of Isolated Cypress Domes to Groundwater Alteration in West-Central Florida
    Evaluating the functional response of isolated cypress domes to groundwater alteration in west-central Florida by Megan Kristine Bartholomew A thesis submitted to the Graduate Faculty of Auburn University in partial fulfillment of the requirements for the Degree of Master of Science Auburn, Alabama May 6, 2017 Copyright 2017 by Megan Bartholomew Approved by Christopher Anderson, Chair, Professor of Wetland Ecology Robert Boyd, Professor of Plant Ecology Jacob Berkowitz, Research Soil Scientist Abstract The hydrology of a wetland is the single most important determinant of its function and slight alterations can lead to significant changes in plant communities and biogeochemistry within the wetland. Therefore, understanding the influence of hydrology on vegetative and soil processes is pivotal to restoration efforts. This study investigated how hydrologic alteration and recovery influenced wetland vegetation and soil processes in Starkey Wilderness Park (SWP), a well-field in west-central Florida. Vegetation responses to groundwater alterations were observed using long term species and hydrologic data collected from SWP. The results from the vegetation study suggest that hydrologic recovery has restored vegetative functions and measures, such as species richness and hydrophytic assemblages, in a relatively short (5-7 year) period. However, differences in species composition and community variation persist in wetlands of various degrees of hydrologic alterations. A field study was also conducted to determine how hydrologic alterations continue to affect wetland decomposition rates and other soil processes. After eight years of hydrologic recovery, altered wetlands experienced faster decomposition than reference wetlands and rates seemed to be linked to differences in both inundation and percent soil organic matter.
    [Show full text]
  • Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44)
    W&M ScholarWorks CCB Technical Reports Center for Conservation Biology (CCB) 1999 Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) B. D. Watts The Center for Conservation Biology, [email protected] Follow this and additional works at: https://scholarworks.wm.edu/ccb_reports Recommended Citation Watts, B. D., "Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44)" (1999). CCB Technical Reports. 454. https://scholarworks.wm.edu/ccb_reports/454 This Report is brought to you for free and open access by the Center for Conservation Biology (CCB) at W&M ScholarWorks. It has been accepted for inclusion in CCB Technical Reports by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) April 1999 Center for Conservation Biology College of William and Mary & Virginia Commonwealth University Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) April 1999 Bryan D. Watts, PhD Center for Conservation Biology College of William and Mary & Virginia Commonwealth University Address comments to: Bryan D. Watts Center for Conservation Biology College of William and Mary Williamsburg, VA 23187-8795 (757) 221-2247 [email protected] Recommended Citation: Watts, B. D. 1999. Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44). Center for Conservation Biology Technical Report Series, CCBTR-99-08. College of William and Mary & Virginia Commonwealth University, Williamsburg, VA. 84 pp. The Center for Conservation Biology is an organization dedicated to discovering innovative solutions to environmental problems that are both scientifically sound and practical within today’s social context.
    [Show full text]
  • Structural and Stratigraphic Framework, and Spatial Distribution of Permeability of the Atlantic Coastal Plain, North Carolina to New York
    Structural and Stratigraphic Framework, and Spatial Distribution of Permeability of the Atlantic Coastal Plain, North Carolina to New York GEOLOGICAL SURVEY PROFESSIONAL PAPER 796 Structural and Stratigraphic Framework, and Spatial Distribution of Permeability of the Atlantic Coastal Plain, North Carolina to New York By PHILIP M. BROWN, JAMES A. MILLER, and FREDERICK M. SWAIN GEOLOGICAL SURVEY PROFESSIONAL PAPER 796 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600285 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 2401-00243 CONTENTS Page Abstract.___________________________________________ 1 Stratigraphic framework Continued Introduction. __ _____________________---____----_-____ 2 Lithostratigraphic description and biostratigraphic Location of area.____________________________________ 3 discussion Continued Acknowledgments. __________________________________ 3 Cenozoic Era__ ____________-_-___--__-------_ 45 Previous work_______________________________________ 5 Tertiary System. _______.-_______----__-_ 45 Purpose of this report. ________________________________ 6 Paleocene Series _ ___________________ 45 Structural architecture._______________________________ 6 Midway Stage Rocks of Midway Introduction, __ ________________________________ 6 Age_ ___----__-____--_------__ 45 General discussion________________________
    [Show full text]
  • Delaware Pennsylvania
    Comparing and Contrasting Delaware and Pennsylvania Name: _________________________ Delaware Delaware, one of America’s original 13 colonies, became America’s first state on December 7, 1787. Hence, its nickname is simply the First State. It became the first state when it ratified, or accepted, the United States Constitution. Delaware is located in the Mid-Atlantic region of the United States, entirely within the Atlantic Coastal Plain. Its capital is Dover and its largest city is Wilmington. Delaware’s land is mostly flat. Its east coast has many wetlands and popular beaches. Delaware is the second smallest state in America in terms of area, and fifth smallest in terms of population. There are less than a million people who live in Delaware. It borders three states: Maryland, Pennsylvania, and New Jersey. Delaware and New Jersey are separated by the wide Delaware River. Pennsylvania Pennsylvania, one of the original 13 colonies, became America’s second state on December 12, 1787. At the time, Philadelphia, Pennsylvania, was the capital of the United States. Millions of people flock to Philadelphia every year to see Independence Hall and the Liberty Bell. Independence Hall was the site of the drafting of both the Declaration of independence and the United States Constitution, two of the most important documents in American history. Gettysburg National Park, located in southern Pennsylvania, was the site of the largest battle ever fought on American soil. The majority of Pennsylvania is covered by the Appalachian Mountains and foothills. Pennsylvania is the only state in the Mid-Atlantic region without beaches. It borders five states: New York, New Jersey, Maryland, West Virginia, and Ohio.
    [Show full text]
  • The Mid-Atlantic Coastal Plain (Physiographic Area 44)
    Partners in Flight Bird Conservation Plan for The Mid-Atlantic Coastal Plain (Physiographic Area 44) Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) VERSION 1.0 April 1999 Address comments to: Bryan D. Watts Center for Conservation Biology College of William and Mary Williamsburg, VA 23187-8795 (757) 221-2247 [email protected] *********************************************** Front cover illustration from ‘All the Birds of North America’ by Jack Griggs, courtesy of HarperCollins publishers. PIF Bird Conservation Plan -- Mid-Atlantic Coastal Plain 2 ACKNOWLEDGMENTS This draft plan was produced with funds provided by the Northern Neck Audubon Society, the Tennessee Conservation League, and the Center for Conservation Biology at the College of William and Mary. I thank Bob Ford and Ken Rosenberg for guidance throughout the planning process. Dana Bradshaw, Mike Wilson, and Marian Watts provided assistance with information and literature. PIF Bird Conservation Plan -- Mid-Atlantic Coastal Plain 3 MID-ATLANTIC COASTAL PLAIN BIRD CONSERVATION PLAN EXECUTIVE SUMMARY The mid-Atlantic Coastal Plain was the site of the first successful European settlement in North America and its landscape has been subject to influence by European culture for nearly four centuries. Currently, the urban crescent from Baltimore south to Richmond and east to Norfolk is experiencing one of the fastest human growth rates in North America. Managing this population growth while maintaining functional natural ecosystems is the greatest conservation challenge faced by land managers within the region. Despite these important management challenges, the potential for successful conservation of priority bird populations remains optimistic. This optimism stems from 1) the fact that a large number of lands critical to priority bird populations are currently protected or held by PIF partners, and 2) many priority species remain relatively abundant and widespread within the region.
    [Show full text]
  • Status of Private Cypress Wetland Forests in Georgia
    STATUS OF PRIVATE CYPRESS WETLAND FORESTS IN GEORGIA Alternatives for Conservation and Restoration ACKNOWLEDGEMENTS We thank the United States Environmental Protection Agency for funding this project, and especially, Jennifer Derby and Tom Welborn for their dedication to conserving Georgia’s cypress resources. We are also grateful to Richard Harper, Jeffery Turner, and Tony Johnson of the U.S. Forest Service, Forest Inventory and Analysis, for their invaluable assistance and train- ing in the retrieval and analysis of the agency’s forest trend data. We thank the Riverkeepers of the Altamaha, Ogeechee, Satilla, and Savannah Rivers for their important contributions to this project. In addition, we wish to express our apprecia- tion to James Holland, the Altamaha Riverkeeper, for the many hours he spent arranging the Wilkinson County case study site visits and working with us in the field to document site conditions. We are grateful to the landowners of the Wilkinson County site for allowing us to evaluate their property and to Mr. Wyndell Berryhall for his assistance in the field. We also wish to thank all those who provided thoughtful review and comments on drafts of this report: Richard Harper, John Greis, Mark Brown, and Tony Johnson of the U.S. Forest Service; Rhett Jackson, Professor of Hydrology, Warnell School of Forestry and Natural Resources, University of Georgia; Frank Green and James Johnson, Georgia Forestry Commission; James Jeter, Ala- bama Forestry Commission; Hughes Simpson, Texas Forest Service; John Swords, U.S. Fish and Wildlife Service; and Shaun Blocker, U.S. Army Corps of Engineers. The Southern Environmental Law Center is a nonprofit organization dedicated to protecting the health and environment of the Southeast (Alabama, Georgia, North Carolina, South Carolina, Tennessee, and Virginia).
    [Show full text]
  • The Effects of Urbanization on the Structure, Quality, and Diversity of Cypress Plant Communities in Central Florida
    University of Central Florida STARS Electronic Theses and Dissertations, 2004-2019 2009 The Effects Of Urbanization On The Structure, Quality, And Diversity Of Cypress Plant Communities In Central Florida Courtney Knickerbocker University of Central Florida Part of the Biology Commons Find similar works at: https://stars.library.ucf.edu/etd University of Central Florida Libraries http://library.ucf.edu This Masters Thesis (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Electronic Theses and Dissertations, 2004-2019 by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Knickerbocker, Courtney, "The Effects Of Urbanization On The Structure, Quality, And Diversity Of Cypress Plant Communities In Central Florida" (2009). Electronic Theses and Dissertations, 2004-2019. 4044. https://stars.library.ucf.edu/etd/4044 THE EFFECTS OF URBANIZATION ON THE STRUCTURE, QUALITY, AND DIVERSITY OF CYPRESS PLANT COMMUNITIES IN CENTRAL FLORIDA by COURTNEY M. KNICKERBOCKER B.A. University of Central Florida, 2002 A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in the Department of Biology In the College of Sciences at the University of Central Florida Orlando, Florida Spring Term 2009 © 2009 Courtney Knickerbocker ii ABSTRACT The integrity of wetland ecosystems is largely determined by hydrological functionality, degree of connectivity to like ecosystems, and permeability to external influence. Land use changes in upland areas adjacent to wetland ecosystems may influence hydrology and connectivity while introducing novel biotic and abiotic materials. There is an increasing trend toward the use of remote assessment techniques to determine the degree of impact of external influences on adjacent wetlands.
    [Show full text]
  • Geologic Framework and Petroleum Potential of the Atlantic Coastal Plain and Continental Shelf
    GEOLOGIC FRAMEWORK AND PETROLEUM POTENTIAL OF THE ATLANTIC COASTAL PLAIN AND CONTINENTAL SHELF ^^^*mmm ^iTlfi".^- -"^ -|"CtS. V is-^K-i- GEOLOGICAL SURVEY PROFESSIONAL PAPER 659 cV^i-i'^S^;-^, - >->"!*- -' *-'-__ ' ""^W^T^^'^rSV-t^^feijS GEOLOGIC FRAMEWORK AND PETROLEUM POTENTLY L OF THE ATLANTIC COASTAL PLAIN AND CONTINENTAL SHELF By JOHN C. MAHBR ABSTRACT less alined with a string of seamounts extending down the continental rise to the abyssal plain. The trends parallel to The Atlantic Coastal Plain and Continental Shelf of North the Appalachians terminate in Florida against a southeasterly America is represented by a belt of Mesozoic and Cenozoic magnetic trend thought by some to represent an extension of rocks, 150 'to 285 miles wide and 2,400 miles long, extending the Ouachita Mountain System. One large anomaly, known as from southern Florida to the Grand Banks of Newfoundland. the slope anomaly, parallels the edge of the .continental shelf This belt of Mesozoic and Cenozoic rocks encompasses an area north of Cape Fear and seemingly represents th** basement of about 400,000 to 450,000 square miles, more than three- ridge located previously by seismic methods. fourths of which is covered by the Atlantic Ocean. The volume Structural contours on the basement rocks, as drawn from of Mesozoic and Cenozoic rocks beneath the Atlantic Coastal outcrops, wells, and seismic data, parallel the Appalachian Plain and Continental Shelf exceeds 450,000 cubic miles, per­ Mountains except in North and South Carolina, where they haps by a considerable amount. More than one-half of this is bulge seaward around the Cape Fear arch, and in Florida, far enough seaward to contain marine source rocks in sufficient where the deeper contours follow the peninsula.
    [Show full text]