Topic B3. Peat Swamp Forests for Adaptation: Potentials and Vulnerability
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Shrub Swamp State Rank: S5 - Secure
Shrub Swamp State Rank: S5 - Secure cover of tall shrubs with Shrub Swamp Communities are a well decomposed organic common and variable type of wetlands soils. If highbush occurring on seasonally or temporarily blueberries are dominant flooded soils; They are often found in the transition zone between emergent the community is likely to marshes and swamp forests; be a Highbush Blueberry Thicket, often occurring on stunted trees. The herbaceous layer of peat. Acidic Shrub Fens are shrub swamps is often sparse and species- peatlands, dominated by poor. A mixture of species might typically low growing shrubs, along include cinnamon, sensitive, royal, or with sphagnum moss and marsh fern, common arrowhead, skunk herbaceous species of Shrub Swamp along shoreline. Photo: Patricia cabbage, sedges, bluejoint grass, bur-reed, varying abundance. Deep Serrentino, Consulting Wildlife Ecologist. swamp candles, clearweed, and Emergent Marshes and Description: Wetland shrubs dominate turtlehead. Invasive species include reed Shallow Emergent Marshes Cottontail, have easy access to the shrubs Shrub Swamps. Shrub height may be from canary grass, glossy alder-buckthorn, are graminoid dominated wetlands with and protection in the dense thickets. The <1m to 5 meters, of uniform height or common buckthorn, and purple <25% cover of tall shrubs. Acidic larvae of many rare and common moth mixed. Shrub density can be variable, loosestrife. Pondshore/Lakeshore Communities are species feed on a variety of shrubs and from dense (>75% cover) to fairly open broadly defined, variable shorelines associated herbaceous plants in shrub (25-75% cover) with graminoid, around open water. Shorelines often swamps throughout Massachusetts. herbaceous, or open water areas between merge into swamps or marshes. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Research 75 (2011) 531–540 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Response of a warm temperate peatland to Holocene climate change in northeastern Pennsylvania Shanshan Cai, Zicheng Yu ⁎ Department of Earth and Environmental Sciences, Lehigh University, 1 West Packer Avenue, Bethlehem, PA 18015, USA article info abstract Article history: Studying boreal-type peatlands near the edge of their southern limit can provide insight into responses of Received 11 September 2010 boreal and sub-arctic peatlands to warmer climates. In this study, we investigated peatland history using Available online 18 February 2011 multi-proxy records of sediment composition, plant macrofossil, pollen, and diatom analysis from a 14C-dated sediment core at Tannersville Bog in northeastern Pennsylvania, USA. Our results indicate that peat Keywords: accumulation began with lake infilling of a glacial lake at ~9 ka as a rich fen dominated by brown mosses. -
Flooding Projections from Elevation and Subsidence Models for Oil Palm Plantations in the Rajang Delta Peatlands, Sarawak, Malaysia
Flooding projections from elevation and subsidence models for oil palm plantations in the Rajang Delta peatlands, Sarawak, Malaysia Flooding projections from elevation and subsidence models for oil palm plantations in the Rajang Delta peatlands, Sarawak, Malaysia Report 1207384 Commissioned by Wetlands International under the project: Sustainable Peatlands for People and Climate funded by Norad May 2015 Flooding projections for the Rajang Delta peatlands, Sarawak Table of Contents 1 Introduction .................................................................................................................... 8 1.1 Land subsidence in peatlands ................................................................................. 8 1.2 Assessing land subsidence and flood risk in tropical peatlands ............................... 8 1.3 This report............................................................................................................. 10 2 The Rajang Delta - peat soils, plantations and subsidence .......................................... 11 2.1 Past assessments of agricultural suitability of peatland in Sarawak ...................... 12 2.2 Current flooding along the Sarawak coast ............................................................. 16 2.3 Land cover developments and status .................................................................... 17 2.4 Subsidence rates in tropical peatlands .................................................................. 23 3 Digitial Terrain Model of the Rajang Delta and coastal -
Maritime Swamp Forest (Typic Subtype)
MARITIME SWAMP FOREST (TYPIC SUBTYPE) Concept: Maritime Swamp Forests are wetland forests of barrier islands and comparable coastal spits and back-barrier islands, dominated by tall trees of various species. The Typic Subtype includes most examples, which are not dominated by Acer, Nyssa, or Fraxinus, not by Taxodium distichum. Canopy dominants are quite variable among the few examples. Distinguishing Features: Maritime Shrub Swamps are distinguished from other barrier island wetlands by dominance by tree species of (at least potentially) large stature. The Typic Subtype is dominated by combinations of Nyssa, Fraxinus, Liquidambar, Acer, or Quercus nigra, rather than by Taxodium or Salix. Maritime Shrub Swamps are dominated by tall shrubs or small trees, particularly Salix, Persea, or wetland Cornus. Some portions of Maritime Evergreen Forest are marginally wet, but such areas are distinguished by the characteristic canopy dominants of that type, such as Quercus virginiana, Quercus hemisphaerica, or Pinus taeda. The lower strata also are distinctive, with wetland species occurring in Maritime Swamp Forest; however, some species, such as Morella cerifera, may occur in both. Synonyms: Acer rubrum - Nyssa biflora - (Liquidambar styraciflua, Fraxinus sp.) Maritime Swamp Forest (CEGL004082). Ecological Systems: Central Atlantic Coastal Plain Maritime Forest (CES203.261). Sites: Maritime Swamp Forests occur on barrier islands and comparable spits, in well-protected dune swales, edges of dune ridges, and on flats adjacent to freshwater sounds. Soils: Soils are wet sands or mucky sands, most often mapped as Duckston (Typic Psammaquent) or Conaby (Histic Humaquept). Hydrology: Most Maritime Swamp Forests have shallow seasonal standing water and nearly permanently saturated soils. Some may rarely be flooded by salt water during severe storms, but areas that are severely or repeatedly flooded do not recover to swamp forest. -
The Mississippi River Delta Basin and Why We Are Failing to Save Its Wetlands
University of New Orleans ScholarWorks@UNO University of New Orleans Theses and Dissertations Dissertations and Theses 8-8-2007 The Mississippi River Delta Basin and Why We are Failing to Save its Wetlands Lon Boudreaux Jr. University of New Orleans Follow this and additional works at: https://scholarworks.uno.edu/td Recommended Citation Boudreaux, Lon Jr., "The Mississippi River Delta Basin and Why We are Failing to Save its Wetlands" (2007). University of New Orleans Theses and Dissertations. 564. https://scholarworks.uno.edu/td/564 This Thesis is protected by copyright and/or related rights. It has been brought to you by ScholarWorks@UNO with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights- holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/or on the work itself. This Thesis has been accepted for inclusion in University of New Orleans Theses and Dissertations by an authorized administrator of ScholarWorks@UNO. For more information, please contact [email protected]. The Mississippi River Delta Basin and Why We Are Failing to Save Its Wetlands A Thesis Submitted to the Graduate Faculty of the University of New Orleans in partial fulfillment of the requirements for the degree of Master of Science in Urban Studies By Lon J. Boudreaux Jr. B.S. Our Lady of Holy Cross College, 1992 M.S. University of New Orleans, 2007 August, 2007 Table of Contents Abstract............................................................................................................................. -
Rapids Lake, Louisville Swamp, And
U.S. Fish & Wildlife Service Forest Trail 0.6 mile loop urban influences. The Carver Rapids Unit, part of Parking Leaving from the asphalt trail below the Rapids the MN Valley State Recreation Area (DNR), is Chaska Unit Minnesota Valley Lake Education and Visitor Center, this mostly level located entirely within the Louisville Swamp Unit. Chaska Athletic Park (City of Chaska) trail courses through oak and hickory forest, with a See regulations issued by the DNR for this location. 725 W 1st St, Chaska, MN 55318 National Wildlife Refuge brief view of a slough connecting to Long Lake. View wood ducks in the slough and listen for frogs calling. Trail Descriptions Carver Riverside Park (City of Carver) State Trail Access 1.0 mi, one way 300 E Main St, Carver, MN 55315 North Hunter Lot Trail 1 mile, one way This straight, level trail goes 1 mile to a junction with Chaska, Rapids Lake & This trail is a mowed service road running from the the MN Valley State Trail to the north. Continue Bluff Park (City of Carver) parking lot on CR11 (Jonathan Carver Pkwy) to the west on the State Access Trail to join the Mazomani 102 Carver Bluffs Parkway, Carver, MN 55315 Louisville Swamp Units northeast, where it ends at the refuge boundary. Trail to the south and loop back to the parking area View native wildflowers, bur oaks, woodpeckers, and at W 145 St. Rapids Lake Unit Trail Map prairie skink in this restored oak savanna. Jonathan Carver Parkway North Hunter Lot MN Valley State Trail (DNR) 5.0 mi, one way 14905 Jonathan Carver Parkway/CR 11, Carver, MN Carver Creek Loop Trail 1.6 miles (loop) From north to south through the refuge, the trail 55315 This trail system has three entry points: Bluff Park, passes the State Access Trail then drops to cross a About the Chaska Unit Ash Street (downtown Carver), and the Rapids Lake bridge over Sand Creek. -
Acid Discharge from the Tropical Peat Swamp Forest and Its Impact on Local People – a Review
TROPICAL PEATLANDS Acid discharge from the tropical peat swamp forest and its impact on local people – a review Akira Haraguchi 1, Liwat Yulintine 2, Linda Wulandari 2, Tris Liana 2, Sepmiarna Welsiana 3 1 The University of Kitakyushu, Hibikino 1-1, Wakamatsu, Kitakyushu 808-0135, Japan Phone: +81 93 695 3291, Fax: +81 93 695 3383, E-mail: [email protected] 2 The University of Palangkaraya, Palangkaraya, Central Kalimantan, Indonesia 3 Marine and Fishery Department, Katingan Regency, Central Kalimantan, Indonesia Summary After destruction of the peat layer over pyrite-containing sediment, pyrite is oxidized and sulphuric acid is produced. Sulphuric acid contaminates soil and river water and then acidifies the environment. Soil chemical and limnological studies in peat swamp forest in Central Kalimantan showed that sulphuric acid loading from acid sulphate soil occurred widely in the coastal region ranging from the river mouth up to 150 km from the coast. The amount of sulphuric acid discharged to freshwater systems was much higher in the rainy season than in the dry season. By holding interviews with local inhabitants on the source of drinking water for inhabitants in polluted areas this was significantly different between dry and rainy seasons. During the rainy season, river and canal water in polluted areas is not available for drinking, and at this time people avoid using river water for drinking. This paper reviews our limnological and biogeochemical studies on acidification of peat by sulphuric acid, discharging process of sulphuric acid to freshwater system, and impact of sulphuric acid pollution on local inhabitants. Key index words : acid sulphate soil, freshwater ecosystem, peat swamp forest, tropical peat, water resource Distribution of pyrite and its impact on Sulphuric acid discharge from acid peat acidification sulphate soil to freshwater ecosystems Pyrite (FeS 2) is formed in a reducing environment, e.g. -
Questioning Ten Common Assumptions About Peatlands
Questioning ten common assumptions about peatlands University of Leeds Peat Club: K.L. Bacon1, A.J. Baird1, A. Blundell1, M-A. Bourgault1,2, P.J. Chapman1, G. Dargie1, G.P. Dooling1,3, C. Gee1, J. Holden1, T. Kelly1, K.A. McKendrick-Smith1, P.J. Morris1, A. Noble1, S.M. Palmer1, A. Quillet1,3, G.T. Swindles1, E.J. Watson1 and D.M. Young1 1water@leeds, School of Geography, University of Leeds, UK 2current address: Centre GEOTOP, CP 8888, Succ. Centre-Ville, Montréal, Québec, Canada 3current address: Geography, College of Life and Environmental Sciences, University of Exeter, UK _______________________________________________________________________________________ SUMMARY Peatlands have been widely studied in terms of their ecohydrology, carbon dynamics, ecosystem services and palaeoenvironmental archives. However, several assumptions are frequently made about peatlands in the academic literature, practitioner reports and the popular media which are either ambiguous or in some cases incorrect. Here we discuss the following ten common assumptions about peatlands: 1. the northern peatland carbon store will shrink under a warming climate; 2. peatlands are fragile ecosystems; 3. wet peatlands have greater rates of net carbon accumulation; 4. different rules apply to tropical peatlands; 5. peat is a single soil type; 6. peatlands behave like sponges; 7. Sphagnum is the main ‘ecosystem engineer’ in peatlands; 8. a single core provides a representative palaeo-archive from a peatland; 9. water-table reconstructions from peatlands provide direct records of past climate change; and 10. restoration of peatlands results in the re-establishment of their carbon sink function. In each case we consider the evidence supporting the assumption and, where appropriate, identify its shortcomings or ways in which it may be misleading. -
Fossil Peat of the Illinois Basin : a Guide to the Study of Coal Balls Of
^uA^^^^i 557 IL6ed no. 11 vol <=>&ued- // FOSSIL PEAT FROM THE ILLINOIS BASIN cn:.\/E' HM * Tom L. Phillips Matthew J. Avcin Dwain Berggren 9lUmH Stcde Qeol(Xjical SuMtey STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION COVER - A photograph (natural size) of a cellulose acetate peel showing the fossil peat preserved in a coal ball collected from the Herrin (No. 6) Coal Member near Carrier Mills, Illinois. Figure 2 describes its contents. 1976 ILLINOIS STATE GEOLOGICAL SURVEY Urbana, Illinois 61801 Jack A. Simon, M.S., Chief ILLINOIS STATE GEOLOGICAL SURVEY ithority of State of Illinois. Ch. 127. IRS. Par. 58 .25 3 3051 00004 8540 I FOSSIL PEAT OF THE ILLINOIS BASIN Goal QalU of PenntyUankM, Acje Tom L. Phillips Matthew J. Avcin Dwain Berggren Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/fossilpeatofilli11phil CONTENTS Introduction 1 Geology of the fossil peat deposits 3 The Illinois Basin 3 How the coal balls formed 3 Plants in fossil peat 7 Studies of fossil peat 9 Internal anatomy and external morphology 10 Plant taxonomy 11 Plant evolution 12 Palynology 13 Preparation of floras 14 Analyses of permineralized peat 14 Formation of coal balls 17 Preparing coal balls for study 17 Making coal-ball peels 18 Examining peels with a microscope 24 Mounting peel sections on glass slides 24 Recovering spores and other microfossils from coal balls 26 Preserving coal balls 28 Repairing and embedding coal-ball slices 29 Sources of materials 31 Finding coal balls 31 Materials needed 32 Selected references 33 Plates and explanations 34 . -
Beje Aquaculture and Inland Fishery in Tropical Peatland of Indonesia
Beje aquaculture and inland fishery in tropical peatland of Indonesia Source Mitigation of Climate Change in Agriculture (MICCA) Programme of FAO Keywords Fisheries, aquaculture, fish production, ponds Country of first practice Indonesia ID and publishing year 8619 and 2016 Sustainable Development Goals No proverty and life below water Summary For many tribes in the tropics (e.g. the between two rivers, and thanks to the soil Kutai and Banjar tribes in East Kalimantan, properties, it forms a kind of water tower Indonesia), fishing in peatland catchments or peat dome (Figure 3), with fully diverse is their main livelihood. Peatlands are their vegetation on the top of it. That is why in the main resources area. They traditionally catch Figure 2, the peatland is higher than the level fishes and reptiles, and collect fuel wood and of the river. In the rainy season it collects grass in peatlands. In January and February, water and in the dry season water is slowly fishes migrate into the waters in the peat released (compare Figure 3). forest for mating and breeding. During this Figure 1. Fishing in a peat swamp forest season fishermen have relatively little catch since most fishes are in the shallow inland waters far inside the peat forest. Fishers using these artificial ponds, called beje, take advantage of fluctuations in the movement of water or overflow of river water during the rainy season from November to March to trap the fish in artificial ponds or special containers. Fish come into the beje by © FAO/TECA themselves since they follow the water flow from the river to the peatland. -
Resolving Cypriniformes Relationships Using an Anchored Enrichment Approach Carla C
Stout et al. BMC Evolutionary Biology (2016) 16:244 DOI 10.1186/s12862-016-0819-5 RESEARCH ARTICLE Open Access Resolving Cypriniformes relationships using an anchored enrichment approach Carla C. Stout1*†, Milton Tan1†, Alan R. Lemmon2, Emily Moriarty Lemmon3 and Jonathan W. Armbruster1 Abstract Background: Cypriniformes (minnows, carps, loaches, and suckers) is the largest group of freshwater fishes in the world (~4300 described species). Despite much attention, previous attempts to elucidate relationships using molecular and morphological characters have been incongruent. In this study we present the first phylogenomic analysis using anchored hybrid enrichment for 172 taxa to represent the order (plus three out-group taxa), which is the largest dataset for the order to date (219 loci, 315,288 bp, average locus length of 1011 bp). Results: Concatenation analysis establishes a robust tree with 97 % of nodes at 100 % bootstrap support. Species tree analysis was highly congruent with the concatenation analysis with only two major differences: monophyly of Cobitoidei and placement of Danionidae. Conclusions: Most major clades obtained in prior molecular studies were validated as monophyletic, and we provide robust resolution for the relationships among these clades for the first time. These relationships can be used as a framework for addressing a variety of evolutionary questions (e.g. phylogeography, polyploidization, diversification, trait evolution, comparative genomics) for which Cypriniformes is ideally suited. Keywords: Fish, High-throughput -
Alaska Non-Timber Forest Products Harvest Manual for Commercial Harvest on State-Owned Lands
Alaska Non-Timber Forest Products Harvest Manual For Commercial Harvest on State-Owned Lands State of Alaska Department of Natural Resources Division of Mining, Land and Water April 2, 2008 - 1 - State of Alaska Non-Timber Forest Product Commercial Harvest Manual, April 2, 2008 Table of Contents Introduction 3 Special notices, clarifications, and general rules 4 Procedure for revision 5 Products and species descriptions 6 Bark birch 7 cedar 8 various species 9 Berries and berry-like fruits 10 Branches and stems of deciduous woody species 11 Buds and tips 12 Burls and galls 13 Cones 14 Conks 15 Cuttings – willow, dogwood & poplar 16 Diamond willow 17 Evergreen boughs 18 Floral greenery 19 Leaves and flowers of woody plants 20 Lichens ground-growing 21 tree-growing 22 Mosses and liverworts 23 Mushrooms 24 Non-woody perennial plants tender edible shoots, stems, leaves, and/or flowers 25 mature stems, leaves and flowers 26 Roots edible or medicinal 27 for fiber 28 Seed heads 29 Seeds 30 Transplants plugs 31 shrubby perennial with root ball 32 sprigs 33 tree sapling with root ball 34 Appendix I: Plants never allowed for harvest 35 Appendix II: Guidelines for non over-the-counter permit products 36 Glossary 38 Selected references 39 - 2 - State of Alaska Non-Timber Forest Product Commercial Harvest Manual, April 2, 2008 Introduction Non-timber forest products are generally defined as products derived from biological resources. Examples of non-timber forest products may include mushrooms, conks, boughs, cones, leaves, burls, landscaping transplants, roots, flowers, fruits, and berries. Not included are minerals, rocks, soil, water, animals, and animal parts.