Landscape Ecosystems of the Fleming Creek Valley, University of Michigan’S Matthaei Botanical Gardens

Total Page:16

File Type:pdf, Size:1020Kb

Landscape Ecosystems of the Fleming Creek Valley, University of Michigan’S Matthaei Botanical Gardens Landscape Ecosystems of the Fleming Creek Valley, University of Michigan’s Matthaei Botanical Gardens Report submitted in completion of research conducted for the Sam Graham’s Trees Project By Alan J. Tepley March 9, 2001 ACKNOWLEDGEMENTS This research was made possible by funding from the Graham Foundation. This research was conducted to provide a sound ecological basis for the grove locations for an interpretive educational trail to honor Dr. Samuel A. Graham, a former professor at the University of Michigan’s School of Natural Resources and Environment. Many individuals have contributed greatly to the success of this research. First, I would like to thank Dr. Burton V. Barnes for his guidance and support, and for his review of drafts of the report. I also would like to thank Dr. David Michener and Dr. Brian Klatt for their advice, encouragement, and for reviewing a draft of the report. Dr. Sylvia Taylor and the rest of the staff at the Matthaei Botanical Gardens also provided encouragement due to their interest in the research. The development of GIS maps would not have been possible without the help of the staff at the Environmental and Spatial Analysis (ESA) lab at the University of Michigan’s School of Natural Resources and Environment. Ecosystems of the Fleming Creek Valley Page-i Ecosystems of the Fleming Creek Valley Page-ii Landscape Ecosystems of the Fleming Creek Valley, University of Michigan’s Matthaei Botanical Gardens ABSTRACT: A landscape ecosystem approach was applied to a 50-ha portion of the Fleming Creek valley at the University of Michigan’s Matthaei Botanical Gardens, Washtenaw County, Michigan. Using an ecological, multifactor approach integrating physiography, hydrology, soil, and vegetation, ecosystems were classified, described, and mapped at three hierarchical levels (Physiographic System, Landform-Level Ecosystem, and Landscape Ecosystem Type). One Physiographic System (Outwash Plain), 2 Landform-Level Ecosystems (Terrace and River Floodplain), and 16 Landscape Ecosystem types were identified, classified, and mapped. Although Fleming Creek is a relatively small stream, the physiographic shape of its valley and the associated pattern of ecosystems are similar to that of many major river valleys. Despite its small area, the Botanical Gardens exhibits a remarkable diversity of ecosystems. The terrace is composed of two ecosystem types, a dry-mesic ecosystem, and a wet depression. The floodplain contains 14 ecosystems, which were ordered into 4 groups; first bottom, second bottom, groundwater seepage, and miscellaneous floodplain features. The ecosystem types of the first bottom include levee, first bottom flat, backswamp, depression, meander-scar marsh, and a wet- mesic ecosystem adjacent to the stream and below upland features. The second bottom contains a moderately well drained ecosystem type on loamy soil, a somewhat poorly drained ecosystem on clay loam to clay soil, and a groundwater seepage on muck. Most of the west side of the floodplain consists of a groundwater seepage that gently slopes from the levee to the terrace. Miscellaneous floodplain features include a deposit of marl overlaid by a thin layer of mineral soil, a crevasse filling, a ridge that remains after a late 19th century or early 20th century excavation, and risers, or steep slopes that separate bottoms or terraces. Within two ecosystem types, the first bottom flat and the groundwater seepage, inclusions, or areas of relatively homogeneous soil and hydrologic conditions, were identified to aid in the interpretation of fine scale variability. Because the Botanical Gardens contains many ecosystem types within a small area, and the pattern of ecosystems represents that of many river valleys, it has high potential for education about the landscape ecosystems of river valleys and their function within the broader landscape. Ecosystems of the Fleming Creek Valley Page-iii Ecosystems of the Fleming Creek Valley Page-iv Table of Contents Page Acknowledgements ................................................................................................................... i Abstract ..................................................................................................................................... iii List of Tables ............................................................................................................................. vi List of Figures ........................................................................................................................... vii List of Appendices ..................................................................................................................... ix Introduction ............................................................................................................................... 1 Objectives ......................................................................................................................... 5 Hierarchical Organization of Ecosystem .......................................................................... 6 Methods ..................................................................................................................................... 9 Study Area ................................................................................................................................. 12 Glacial History .................................................................................................................. 12 Postglacial Influences on Fleming Creek Valley Geomorphology ................................... 17 Results and Discussion.............................................................................................................. 19 Overview of the Classification ......................................................................................... 19 Inclusions within Landscape Ecosystem Types ................................................................ 27 Physiographic Pattern and the Correspondence of Species.............................................. 30 River Valley............................................................................................................. 35 River Floodplain..................................................................................................... 37 General Discussion ................................................................................................................... 42 Levels of Classification .................................................................................................... 42 Presettlement Vegetation .................................................................................................. 43 Michigan Natural Features Inventory Community Types ...................................... 46 Similarities to Other River Valleys................................................................................... 48 Terrace .................................................................................................................... 48 Levee ....................................................................................................................... 49 First Bottom ............................................................................................................ 49 Second Bottom ........................................................................................................ 53 Alterations of the Landscape ............................................................................................ 54 Ecosystem Diversity ......................................................................................................... 55 Flood Control and the Lack of Fire .................................................................................. 56 Death of American elm and Tamarack ............................................................................. 61 Summary and Conclusions ....................................................................................................... 65 Ecosystems of the Fleming Creek Valley Page-v List of Tables Page Table 1. Classification of the landscape ecosystems and their corresponding 20 presettlement cover types within a segment of the Fleming Creek Valley, University of Michigan’s Matthaei Botanical Gardens. Washtenaw Co., Michigan Table 2. Community composition of the first bottom flat. University of 58 Michigan's Matthaei Botanical Gardens. Washtenaw Co., Michigan. Table 3. Correspondence of overstory and understory vegetation to ecosystem 60 type along a moisture gradient in the ecosystems of the second bottom. University of Michigan's Matthaei Botanical Gardens. Washtenaw Co., Michigan. Table 4. Present community structure in ecosystems formerly occupied by 64 American elm and eastern larch. University of Michigan's Matthaei Botanical Gardens. Washtenaw Co., Michigan. Ecosystems of the Fleming Creek Valley Page-vi List of Figures Page Figure 1. Map of the regional landscape ecosystems of Lower Michigan (a) 7 (Albert et al. 1986). Roman numerals indicate Regions, divided by a thick dark line. Within each region, Districts and Subdistricts are indicated by thinner lines, as well as integers and decimals, respectively. The location of the University of Michigan’s Matthaei Botanical Gardens is indicated by a star. Hierarchical organization of regional and local landscape ecosystems (b), with a generalized classification of the ecosystems of the Botanical Gardens superimposed on the progression from regional to local ecosystems.
Recommended publications
  • Missouri River Floodplain from River Mile (RM) 670 South of Decatur, Nebraska to RM 0 at St
    Hydrogeomorphic Evaluation of Ecosystem Restoration Options For The Missouri River Floodplain From River Mile (RM) 670 South of Decatur, Nebraska to RM 0 at St. Louis, Missouri Prepared For: U. S. Fish and Wildlife Service Region 3 Minneapolis, Minnesota Greenbrier Wetland Services Report 15-02 Mickey E. Heitmeyer Joseph L. Bartletti Josh D. Eash December 2015 HYDROGEOMORPHIC EVALUATION OF ECOSYSTEM RESTORATION OPTIONS FOR THE MISSOURI RIVER FLOODPLAIN FROM RIVER MILE (RM) 670 SOUTH OF DECATUR, NEBRASKA TO RM 0 AT ST. LOUIS, MISSOURI Prepared For: U. S. Fish and Wildlife Service Region 3 Refuges and Wildlife Minneapolis, Minnesota By: Mickey E. Heitmeyer Greenbrier Wetland Services Advance, MO 63730 Joseph L. Bartletti Prairie Engineers of Illinois, P.C. Springfield, IL 62703 And Josh D. Eash U.S. Fish and Wildlife Service, Region 3 Water Resources Branch Bloomington, MN 55437 Greenbrier Wetland Services Report No. 15-02 December 2015 Mickey E. Heitmeyer, PhD Greenbrier Wetland Services Route 2, Box 2735 Advance, MO 63730 www.GreenbrierWetland.com Publication No. 15-02 Suggested citation: Heitmeyer, M. E., J. L. Bartletti, and J. D. Eash. 2015. Hydrogeomorphic evaluation of ecosystem restoration options for the Missouri River Flood- plain from River Mile (RM) 670 south of Decatur, Nebraska to RM 0 at St. Louis, Missouri. Prepared for U. S. Fish and Wildlife Service Region 3, Min- neapolis, MN. Greenbrier Wetland Services Report 15-02, Blue Heron Conservation Design and Print- ing LLC, Bloomfield, MO. Photo credits: USACE; http://statehistoricalsocietyofmissouri.org/; Karen Kyle; USFWS http://digitalmedia.fws.gov/cdm/; Cary Aloia This publication printed on recycled paper by ii Contents EXECUTIVE SUMMARY ....................................................................................
    [Show full text]
  • Chapter 5 Groundwater Quality and Hydrodynamics of an Acid Sulfate Soil Backswamp
    Chapter 5 Groundwater Quality and Hydrodynamics of an Acid Sulfate Soil Backswamp 5.1 Introduction Intensive drainage of coastal floodplains has been the main factor contributing to the oxidation of acid sulfate soils (ASS) (Indraratna, Blunden & Nethery 1999; Sammut, White & Melville 1996). Drainage of backswamps removes surface water, thereby increasing the effect of evapotranspiration on watertable drawdown (Blunden & Indraratna 2000) and transportation of acidic salts to the soil surface through capillary action (Lin, Melville & Hafer 1995; Rosicky et al. 2006). During high rainfall events the oxidation products (i.e. metals and acid) are mobilised into the groundwater, and acid salts at the sediment surface are dissolved directly into the surface water (Green et al. 2006). The high efficiency of drains readily transports the acidic groundwater and surface water into the estuary and can have a detrimental impact on downstream habitats (Cook et al. 2000). The quality of water discharged from a degraded ASS wetland is controlled by the water balance, which over a given time period is: P + I + Li = E + Lo + D + S (Equation 5.1) where P is precipitation, I is irrigation, Li is the lateral inflow of water, E is evapotranspiration, Lo is surface and subsurface lateral outflow of water, D is the drainage to the watertable and S is the change in soil moisture storage above the watertable (Indraratna, Tularam & Blunden 2001; Sammut, White & Melville 1996; White et al. 1997). While this equation may give a general overview of sulfidic floodplain hydrology, an understanding of site-specific details is required for effective remediation and management of degraded ASS wetlands.
    [Show full text]
  • Cypress Creek National Wildlife Refuge, Illinois
    Hydrogeomorphic Evaluation of Ecosystem Restoration Options for Cypress Creek National Wildlife Refuge, Illinois Prepared For: U. S. Fish and Wildlife Service Division of Refuges, Region 3 Minneapolis, Minnesota Greenbrier Wetland Services Report 12-05 Mickey E. Heitmeyer Karen E. Mangan July 2012 HYDROGEOMORPHIC EVALUATION OF ECOSYSTEM RESTORATION OPTIONS FOR CYPRESS CREEK NATIONAL WILDLIFE REFUGE, ILLINOIS Prepared For: U.S. Fish and Wildlife Service National Wildlife Refuge System, Region 3 Minneapolis, MN and Cypress Creek National Wildlife Refuge Ullin, IL By: Mickey E. Heitmeyer, PhD Greenbrier Wetland Services Rt. 2, Box 2735 Advance, MO 63730 and Karen E. Mangan U.S. Fish and Wildlife Service Cypress Creek National Wildlife Refuge 0137 Rustic Campus Drive Ullin, IL 62992 Greenbrier Wetland Services Report 12-05 July 2012 Mickey E Heitmeyer, PhD Greenbrier Wetland Services Route 2, box 2735 Advance, MO. 63730 Publication No. 12-05 Suggested citation: Heitmeyer, M. E., K. E. Mangan. 2012. Hy- drogeomorphic evaluation of ecosystem restora- tion and management options for Cypress Creek National Wildlife Refuge,Ullin Il.. Prepared for U. S. Fish and Wildlife Service, Region 3, Minne- apolis, MN and Cypress Creek National Wildlife Refuge,Ullin,Il. Greenbrier Wetland Services Report 12-05, Blue Heron Conservation Design and Printing LLC, Bloomfield, MO. Photo credits: COVER: Limekiln Slough by Michael Jeffords Michael Jeffords, Jan Sundberg, Cary Aloia (Gardners- Gallery.com), Karen Kyle This publication printed on recycled paper by ii
    [Show full text]
  • Floodplain Geomorphic Processes and Environmental Impacts of Human Alteration Along Coastal Plain Rivers, Usa
    WETLANDS, Vol. 29, No. 2, June 2009, pp. 413–429 ’ 2009, The Society of Wetland Scientists FLOODPLAIN GEOMORPHIC PROCESSES AND ENVIRONMENTAL IMPACTS OF HUMAN ALTERATION ALONG COASTAL PLAIN RIVERS, USA Cliff R. Hupp1, Aaron R. Pierce2, and Gregory B. Noe1 1U.S. Geological Survey 430 National Center, Reston, Virginia, USA 20192 E-mail: [email protected] 2Department of Biological Sciences, Nicholls State University Thibodaux, Louisiana, USA 70310 Abstract: Human alterations along stream channels and within catchments have affected fluvial geomorphic processes worldwide. Typically these alterations reduce the ecosystem services that functioning floodplains provide; in this paper we are concerned with the sediment and associated material trapping service. Similarly, these alterations may negatively impact the natural ecology of floodplains through reductions in suitable habitats, biodiversity, and nutrient cycling. Dams, stream channelization, and levee/canal construction are common human alterations along Coastal Plain fluvial systems. We use three case studies to illustrate these alterations and their impacts on floodplain geomorphic and ecological processes. They include: 1) dams along the lower Roanoke River, North Carolina, 2) stream channelization in west Tennessee, and 3) multiple impacts including canal and artificial levee construction in the central Atchafalaya Basin, Louisiana. Human alterations typically shift affected streams away from natural dynamic equilibrium where net sediment deposition is, approximately, in balance with net
    [Show full text]
  • Classifying Rivers - Three Stages of River Development
    Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion.
    [Show full text]
  • Stream Channel and Vegetation Monitoring Reportreport,,,, 2005 Through 2008
    Resurrection Creek Stream and Riparian Restoration Project Stream Channel and Vegetation Monitoring ReportReport,,,, 2005 through 2008 USDA Forest Service Chugach National Forest January 2009 Resurrection Creek Restoration Monitoring Report January 2009 Resurrection Creek Stream and Riparian Restoration Project Stream Channel and Vegetation Monitoring Report 2005 through 2008 USDA Forest Service Chugach National Forest Seward Ranger District Bill MacFarlane, Chugach National Forest Hydrologist Rob DeVelice, Chugach National Forest Ecologist Dean Davidson, Chugach National Forest Soil Scientist (retired) January 2009 1 Resurrection Creek Restoration Monitoring Report January 2009 Summary______________________________________________________________ The Resurrection Creek Stream Restoration project was implemented in 2005 and 2006, with project area revegetation continuing through 2008. Stream channel morphology and vegetation have been monitored in 2005, 2006, 2007, and 2008. This report compiles the 2008 data and summarizes the 4 years of monitoring data and the short-term response of the project area to the restoration. Each of the project objectives established prior to the implementation of this project were fully or partially accomplished. These included variables that quantify channel pattern, channel profile, side channels, aquatic habitat, and riparian vegetation. While the target values may not have been met in all cases, the intent of each objective was met through restoration. The response of the project area in the 3 years following restoration represents the short- term response to restoration. While numerous changes can occur in this period as the morphology and vegetation adjusts to the new conditions, no major channel changes have occurred on Resurrection Creek or its side channels, and vegetation growth in the riparian area has occurred as expected.
    [Show full text]
  • Johnson Creek Restoration Project Effectiveness Monitoring
    Bureau of Environmental Services • City of Portland Johnson Creek Restoration Projects Effectiveness Monitoring Reporting on data collected from 1997 through 2010 DECEMBER 2012 Dan Saltzman, Commissioner Dean Marriott, Director Dan Saltzman, Commissioner • Dean Marriott, Director Acknowledgements Implementation of the effectiveness monitoring program for restoration projects in the Johnson Creek Watershed has drawn on the expertise, support, and dedication of a number of individuals. We thank them for making this report possible. City of Portland, Environmental Services Staff Jennifer Antak, Johnson Creek Effectiveness Monitoring Program Lead Sean Bistoff Trevor Diemer Mathew Dorfman Steven Kass Theophilus Malone Chris Prescott Gregory Savage Wendy Sletten Maggie Skenderian Ali Young Supporting Organizations and Consultants Oregon Watershed Enhancement Board Salmon River Engineering ‐ Janet Corsale, PE CPESC Portland State University ‐ Denisse Fisher Contents Introduction .........................................................................................................................1 Johnson Creek Overview ...................................................................................................1 Project Effectiveness Monitoring Program....................................................................12 Overview ........................................................................................................................12 Monitoring Methods.....................................................................................................13
    [Show full text]
  • Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota Dylan Babiracki
    University of North Dakota UND Scholarly Commons Undergraduate Theses and Senior Projects Theses, Dissertations, and Senior Projects 2015 Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota Dylan Babiracki Follow this and additional works at: https://commons.und.edu/senior-projects Recommended Citation Babiracki, Dylan, "Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota" (2015). Undergraduate Theses and Senior Projects. 114. https://commons.und.edu/senior-projects/114 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Undergraduate Theses and Senior Projects by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. | 1 Lateral migration of the Red River, in the vicinity of Grand Forks, North Dakota Dylan Babiracki Harold Hamm School of Geology and Geologic Engineering, University of North Dakota, 81 Cornell St., Grand Forks, ND 58202-8358 1. Abstract River channels are dynamic landforms that play an important role in understanding the alluvial changes occurring within this area. The evolution of the Red River of the North within the shallow alluvial valley was investigated within a 60 river mile area north and south of Grand Forks, North Dakota. Despite considerable research along the Red River of the North, near St. Jean Baptiste, Manitoba, little is known about the historical channel dynamics within the defined study area. A series of 31 measurements were taken using three separate methods to document the path of lateral channel migration along areas of this highly sinuous, low- gradient river.
    [Show full text]
  • EARTH SCIENCES RESEARCH JOURNAL Development of Tropical
    EARTH SCIENCES RESEARCH JOURNAL Earth Sci. Res. J. Vol. 20, No. 1 (March, 2016): O1 - O10 GEOLOGY ENGINEERING Development of Tropical Lowland Peat Forest Phasic Community Zonations in the Kota Samarahan-Asajaya area, West Sarawak, Malaysia Mohamad Tarmizi Mohamad Zulkifley1, Ng Tham Fatt1, Zainey Konjing2, Muhammad Aqeel Ashraf3,4* 1. Department of Geology, Faculty of Science, University of Malaya, Kuala Lumpur, Malaysia 2. Biostratex Sendirian Berhad, Batu Caves, Gombak, Malaysia. 3. Department of Environmental Science and Engineering, School of Environmental Studies, China University of Geosciences, 430074 Wuhan, P. R. China 4. Faculty of Science & Natural Resources, University Malaysia Sabah88400 Kota Kinabalu, Sabah, Malaysia. Corresponding authors: Muhammad Aqeel Ashraf- Faculty of Science & Natural Resources University Malaysia Sabah, 88400, Kota Kinabalu, Sabah. ([email protected]) ABSTRACT Keywords: Lowland peat swamp, Phasic community, Logging observations of auger profiles (Tarmizi, 2014) indicate a vertical, downwards, general decrease of Mangrove swamp, Riparian environment, Pollen peat humification levels with depth in a tropical lowland peat forest in the Kota Samarahan-Asajaya área in the diagram, Vegetation Succession. región of West Sarawak (Malaysia). Based on pollen analyses and field observations, the studied peat profiles can be interpreted as part of a progradation deltaic succession. Continued regression of sea levels, gave rise Record to the development of peat in a transitional mangrove to floodplain/floodbasin environment, followed by a shallow, topogenic peat depositional environment with riparian influence at approximately 2420 ± 30 years B.P. Manuscript received: 20/10/2015 (until present time). The inferred peat vegetational succession reached Phasic Community I at approximately Accepted for publication: 12/02/2016 2380 ± 30 years B.P.
    [Show full text]
  • Glossary Ablation Till: Till Carried on Or Near the Surface of a Glacial Ice Column and Let Down As the Glacier Melted and Retreated
    Glossary ablation till: till carried on or near the surface of a glacial ice column and let down as the glacier melted and retreated. alluvium: any mineral or detrital sediment that is transported and deposited by the flowing water of a river or stream. Riverbeds, floodplains, and deltas are all made up of alluvium. backswamp: low-lying wet areas on river floodplains, located away from the active river channel. basal till: till carried in the base of a glacial ice column and deposited under the glacier. Basal till is therefore very dense and typically forms a layer that impedes drainage. biological diversity (biodiversity): the complexity of all life at all its levels of organization, including genetic variability within species, species and species interac- tions, ecological processes, and the distribution of species and natural communities across the landscape. bog: an acidic, peat-accumulating wetland that is isolated from mineral-rich water sources by deep peat accumulation and therefore receives most of its water and nutri- ents from precipitation. Bogs are dominated by sphagnum moss and heath family shrubs. boreal forest: a circumpolar band of northern forests bordered to the north by open tundra and to the south by more transitional forests. Boreal forests are characterized by species of pine, spruce, fir, tamarack, birch, and poplar that are adapted to the extreme cold of this region. bryophyte: a division of plants including the mosses, liverworts, and hornworts. calciphile: a plant that thrives in calcium-rich soils. circumneutral: having a pH near 7.0 and therefore neither strongly acidic nor basic. cliff: an exposed, steep face of rock.
    [Show full text]
  • La Mare a Bore at Center Left
    Geographies of New Orleans A 'Lake' in Broadmoor? Natural Paradise Once Graced Uptown's Last Open Tract Richard Campanella Contributing writer, GEOGRAPHIES OF NEW ORLEANS Published in the Times-Picayune/New Orleans Advocate, November 1, 2020, page A1 Conversations with older residents of the Broadmoor and Fontainebleau neighborhoods often prompt recollections of a “lake” in that vicinity prior to its urbanization. Indeed, a 1922 aerial photograph shows a large undeveloped tract—the last in the area—between Jefferson and Nashville avenues, going back from South Claiborne Avenue to Gert Town. Having subsided to a few feet below sea level, those open fields probably accumulated runoff after heavy rains, creating what looked like what many secondary sources describe as a “twelve-acre lake” in Broadmoor. But if we go back a century earlier, there turns out to be more to the story than a muddy field. Descriptive evidence comes from the pen of famed lawyer and narrative historian Charles Gayarré, who grew up on the plantation encompassing that low spot, and wrote of his memories in an 1886 Harper’s New Monthly Magazine article titled “A Louisiana Sugar Plantation of the Old Regime.” Gayarré was the grandson of Etienne de Boré, the man widely credited—thanks in part to Gayarré’s own dramatized recounting—with figuring out how to granulate locally grown sugarcane juice. That 1795 breakthrough led to a massive expansion of sugar cultivation in lower Louisiana, and of the institution of slavery on which it depended. De Bore’s plantation extended from the present-day 6000 to 6300 blocks of Tchoupitoulas Street straight back to what is now the intersection of Nashville Avenue and Earhart Expressway, an area that includes the aforementioned tract that was still undeveloped as of 1922.
    [Show full text]
  • Coastal Backswamps: Restoring Their Values…
    Note This document contains information from sources other than NSW Agriculture. To preserve the original text no editing has been performed and no alterations to the original format have been made. Recognising that the information is provided by third parties, the State of New South Wales and the publisher take no responsibility for the accuracy, currency, reliability and correctness of any information included in the document. Coastal Backswamps: Restoring their values… Backswamps - before drainage Fauna and flora When the Europeans first settled the east coast of Backswamps were important habitat and nutrient Australia, they found many backswamps along the sources for aquatic life, both within the swamp and in floodplains. Coastal backswamps are the lowest the channels that linked them to the estuary at higher lying areas of a coastal floodplain, generally below flows. Backswamps were major habitat and nursery mean high tide. areas for many fish species. Water cycle Backswamps were also prolific areas for duck and other water birds. Landholders enjoyed the abundant Wet/dry cycle waterfowl and fish that provided food for the table as well as employment for professional duck hunters In most years, backswamps experienced a natural and fishermen. wet/dry cycle according to seasonal rainfall and evaporation. The ecology of backswamps has evolved to cope with these conditions, with wetland Management then or dryland plant species colonising the backswamp margins according to longer-term seasonal Burning conditions. Backswamps did burn pre European occupation, but at frequencies which left them with their natural Natural Drainage vegetation cover of reed and rush largely intact. Backswamps generally held waters for 3-6 months Because back-swamps were wet beneath the surface during and following the wet season.
    [Show full text]