SUMMARY: RSPO MANUAL on BEST MANAGEMENT PRACTICES (Bmps)
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Brodhead Watershed Conservation Plan
Brodhead Watershed Conservation Plan January, 2002 Prepared by: Brodhead Watershed Association With: BLOSS Associates Brodhead Watershed Conservation Plan Acknowledgements The Watershed Partners were the backbone of this planning process. Their commitment to preserving and protecting the watershed underlies this entire plan. Watershed Partners / Conservation Plan Steering Committee Monroe County Commissioners – Mario Scavello, Donna Asure, James Cadue, Former Commissioner Janet Weidensaul Monroe County Conservation District – Craig Todd, Darryl Speicher Monroe County Planning Commission – John Woodling, Eric Bartolacci Monroe County Historical Association – Candace McGreevey Monroe County Office of Emergency Management – Harry Robidoux Monroe County Open Space Advisory Board – Tom O’Keefe Monroe County Recreation & Park Commission – Kara Derry Monroe 2020 Executive Committee – Charles Vogt PA Department of Environmental Protection – Bill Manner Pennsylvania State University – Jay Stauffer Penn State Cooperative Extension – Peter Wulfhurst Stroudsburg Municipal Authority – Ken Brown Mount Pocono Borough – Nancy Golowich Pocono/Hamilton/Jackson Open Space Committee – Cherie Morris Stroud Township – Ross Ruschman, Ed Cramer Smithfield Township – John Yetter Delaware River Basin Commission – Pamela V’Combe, Carol Collier U.S. Environmental Protection Agency – Susan McDowell Delaware Water Gap National Recreation Area – Denise Cook National Park Service, Rivers & Trails Office – David Lange National Institute for Environmental Renewal (no longer -
Comparison of Swamp Forest and Phragmites Australis
COMPARISON OF SWAMP FOREST AND PHRAGMITES AUSTRALIS COMMUNITIES AT MENTOR MARSH, MENTOR, OHIO A Thesis Presented in Partial Fulfillment of the Requirements for The Degree Master of Science in the Graduate School of the Ohio State University By Jenica Poznik, B. S. ***** The Ohio State University 2003 Master's Examination Committee: Approved by Dr. Craig Davis, Advisor Dr. Peter Curtis Dr. Jeffery Reutter School of Natural Resources ABSTRACT Two intermixed plant communities within a single wetland were studied. The plant community of Mentor Marsh changed over a period of years beginning in the late 1950’s from an ash-elm-maple swamp forest to a wetland dominated by Phragmites australis (Cav.) Trin. ex Steudel. Causes cited for the dieback of the forest include salt intrusion from a salt fill near the marsh, influence of nutrient runoff from the upland community, and initially higher water levels in the marsh. The area studied contains a mixture of swamp forest and P. australis-dominated communities. Canopy cover was examined as a factor limiting the dominance of P. australis within the marsh. It was found that canopy openness below 7% posed a limitation to the dominance of P. australis where a continuous tree canopy was present. P. australis was also shown to reduce diversity at sites were it dominated, and canopy openness did not fully explain this reduction in diversity. Canopy cover, disturbance history, and other environmental factors play a role in the community composition and diversity. Possible factors to consider in restoring the marsh are discussed. KEYWORDS: Phragmites australis, invasive species, canopy cover, Mentor Marsh ACKNOWLEDGEMENTS A project like this is only possible in a community, and more people have contributed to me than I can remember. -
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. -
Alternative Stable States of Tidal Marsh Vegetation Patterns and Channel Complexity
ECOHYDROLOGY Ecohydrol. (2016) Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/eco.1755 Alternative stable states of tidal marsh vegetation patterns and channel complexity K. B. Moffett1* and S. M. Gorelick2 1 School of the Environment, Washington State University Vancouver, Vancouver, WA, USA 2 Department of Earth System Science, Stanford University, Stanford, CA, USA ABSTRACT Intertidal marshes develop between uplands and mudflats, and develop vegetation zonation, via biogeomorphic feedbacks. Is the spatial configuration of vegetation and channels also biogeomorphically organized at the intermediate, marsh-scale? We used high-resolution aerial photographs and a decision-tree procedure to categorize marsh vegetation patterns and channel geometries for 113 tidal marshes in San Francisco Bay estuary and assessed these patterns’ relations to site characteristics. Interpretation was further informed by generalized linear mixed models using pattern-quantifying metrics from object-based image analysis to predict vegetation and channel pattern complexity. Vegetation pattern complexity was significantly related to marsh salinity but independent of marsh age and elevation. Channel complexity was significantly related to marsh age but independent of salinity and elevation. Vegetation pattern complexity and channel complexity were significantly related, forming two prevalent biogeomorphic states: complex versus simple vegetation-and-channel configurations. That this correspondence held across marsh ages (decades to millennia) -
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. -
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. -
Occurrence of Fungi on Tissues of the Peat Swamp Palm Licuala Longicalycata
Fungal Diversity Occurrence of fungi on tissues of the peat swamp palm Licuala longicalycata Umpava Pinruan1, Kevin D. Hyde2*, Saisamorn Lumyong1, E.H.C. McKenzie3 and E.B. Gareth Jones4 1Department of Microbiology, Faculty of Science, Chiang Mai University, Chiang Mai, Thailand 50200 2Centre for Research in Fungal Diversity, Department of Ecology & Biodiversity, The University of Hong Kong, Pokfulam Road, Hong Kong SAR, PR China 3Landcare Research, Private Bag 92170, Auckland, New Zealand 4National Center for Genetic Engineering and Biotechnology, 113 Thailand Science Park, Paholyothin Road, Khlong 1, Khlong Luang, Pathum Thani, Thailand 12120 Pinruan, U., Hyde, K.D., Lumyong, S., McKenzie, E.H.C. and E.B.G. Jones (2007). Occurrence of fungi on tissues of the peat swamp palm Licuala longicalycata. Fungal Diversity 25: 157-173. The biodiversity of fungi from decaying palm material of Licuala longicalycata was studied following six field collections in May, June, September and November 2001, and February and May 2002. One-hundred and seventy-seven fungal collections were identified to species level, 153 collections to generic level, while 28 collections remained unidentified. A total of 147 species were identified, including 79 ascomycetes in 50 genera (53%), 65 anamorphic taxa in 53 genera (45%) and 3 basidiomycete species in 3 genera (2%). Nine ascomycetes and 5 anamorphic fungi were new to science. The percentage of fungi occurring in different microhabitats were as follows: dry material supported the most fungi with 40%, submerged material had 32%, while the damp material supported the least number of fungi (28%). The percentage occurrence of fungi on different tissues of L. -
Western Samoa
A Directory of Wetlands in Oceania In: Scott, D.A. (ed.) 1993. A Directory of Wetlands in Oceania. IWRB, Slimbridge, U.K. and AWB, Kuala Lumpur, Malaysia. A Directory of Wetlands in Oceania WESTERN SAMOA INTRODUCTION by Cedric Schuster Department of Lands and Environment Area: 2,935 sq.km. Population: 170,000. Western Samoa is an independent state in the South Pacific situated between latitudes 13° and 14°30' South and longitudes 171° and 173° West, approximately 1,000 km northeast of Fiji. The state comprises two main inhabited islands, Savai'i (1,820 sq.km) and Upolu (1,105 sq.km), and seven islets, two of which are inhabited. Western Samoa is an oceanic volcanic archipelago that originated in the Pliocene. The islands were formed in a westerly direction with the oldest eruption, the Fagaloa volcanics, on the eastern side. The islands are still volcanically active, with the last two eruptions being in 1760 and 1905-11 respectively. Much of the country is mountainous, with Mount Silisili (1,858 m) on Savai'i being the highest point. Western Samoa has a wet tropical climate with temperatures ranging between 17°C and 34°C and an average temperature of 26.5°C. The temperature difference between the rainy season (November to March) and the dry season (May to October) is only 2°C. Rainfall is heavy, with a minimum of 2,000 mm in all places. The islands are strongly influenced by the trade winds, with the Southeast Trades blowing 82% of the time from April to October and 54% of the time from May to November. -
Preliminary Findings on Impact of Logging on Plant Structure and Potential Indicator on Gap Opening in Peat Swamp Forest
International Journal of Chemical, Environmental & Biological Sciences (IJCEBS) Volume 1, Issue 2 (2013) ISSN 2320 –4087 (Online) Preliminary Findings on Impact of Logging on Plant Structure and Potential Indicator on Gap Opening in Peat Swamp Forest Mohd Ghazali, H., Marryanna, L., Ismail, P., Abd Rahman, K., Abdul Razak, O., Salleh, M. and Saiful, I.K. Various parameters may have cause changing of tree Abstract—Various parameters may have cause changing of plant vigorosity especially in PSF. Gap opening might minimize the structure especially in peat swamp forest (PSF). One major cause of trees competition with each other for nutrients, moisture and plant structure changes in the PSF might be logging activities to sunlight. However, some of the species will eventually extract valuable timbers out of the area. The logging activities will dominate and their growth will become the indicators for the create gap opening that minimize competition among the plants for nutrients, moisture and sunlight. Some of the plants will eventually soil properties and water quality in the area. Soil of the area dominate and vigorously growth compared to other species. Just after was developed from organic materials. The soil classification the logging, pioneer plant species grow vigorously due to lower stand detail as in Table I. density and abundance of sunlight. Therefore the presence of these TABLE I species can be attributed to the changes on soil properties and water SOIL SERIES IN STUDY SITE quality of the area. This study is aimed to find possible indicators Soil series Malaysian Soil FAO/UNESCO contributing to this phenomenon. These were done by setting plots in Taxonomy areas with different years after the logging. -
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 . -
Trial by Fire F Orest F Ires and F Orestry P Olicy in I Ndonesia’ S E Ra of C Risis and R Eform
TRIAL BY FIRE F OREST F IRES AND F ORESTRY P OLICY IN I NDONESIA’ S E RA OF C RISIS AND R EFORM CHARLES VICTOR BARBER JAMES SCHWEITHELM WORLD RESOURCES INSTITUTE FOREST FRONTIERS INITIATIVE IN COLLABORATION WITH WWF-INDONESIA & TELAPAK INDONESIA FOUNDATION INDONESIA’S FOREST COVER Notes: (a) Hotspots, showing ground thermal activity detected with the NOAA AVHRR sensor, represent an area of approximately 1 square kilometer. Data from August - December 1997 were processed by IFFM-GTZ, FFPCP (b) Forest cover is from The Last Frontier Forests, Bryant, Nielsen, and Tangley, 1997. "Frontier forest" refers to large, ecologically intact and relatively undisturbed natural forests. "Non-frontier forests" are dominated by eventually degrade the ecosystem. See Bryant, Nielsen, and Tangley for detailed definitions. AND 1997-98 FIRE HOT SPOTS CA, and FFPMP-EU. ondary forests, plantations, degraded forest, and patches of primary forest not large enough to qualify as frontier forest. "Threatened frontier forests" are forests where ongoing or planned human activities will TRIAL BY FIRE F OREST F IRES AND F ORESTRY P OLICY IN I NDONESIA’ S E RA OF C RISIS AND R EFORM CHARLES VICTOR BARBER JAMES SCHWEITHELM WORLD RESOURCES INSTITUTE FOREST FRONTIERS INITIATIVE IN COLLABORATION WITH WWF-INDONESIA & TELAPAK INDONESIA FOUNDATION TO COME Publications Director Hyacinth Billings Production Manager Designed by: Papyrus Design Group, Washington, DC Each World Resources Institute report represents a timely, scholarly treatment of a subject of public concern. WRI takes responsibility for choosing the study topics and guaranteeing its authors and researchers freedom of inquiry. It also solicits and responds to the guidance of advisory panels and expert reviewers. -
PLTA-0103 Nature Conservancy 3/19/04 4:00 PM Page 1
PLTA-0103 Nature Conservancy 3/19/04 4:00 PM Page 1 ............................................................. Pennsylvania’s Land Trusts The Nature Conservancy About Land Trusts Conservation Options Conserving our Commonwealth Pennsylvania Chapter Land trusts are charitable organizations that conserve land Land trusts and landowners as well as government can by purchasing or accepting donations of land and conservation access a variety of voluntary tools for conserving special ................................................................ easements. Land trust work is based on voluntary agreements places. The basic tools are described below. The privilege of possessing Produced by the the earth entails the Pennsylvania Land Trust Association with landowners and creating projects with win-win A land trust can acquire land. The land trust then responsibility of passing it on, working in partnership with outcomes for communities. takes care of the property as a wildlife preserve, the better for our use, Pennsylvania’s land trusts Nearly a hundred land trusts work to protect important public recreation area or other conservation purpose. not only to immediate posterity, but to the unknown future, with financial support from the lands across Pennsylvania. Governed by unpaid A landowner and land trust may create an the nature of which is not William Penn Foundation, Have You Been to the Bog? boards of directors, they range from all-volunteer agreement known as a conservation easement. given us to know. an anonymous donor and the groups working in a single municipality The easement limits certain uses on all or a ~ Aldo Leopold Pennsylvania Department of Conservation n spring days, the Tannersville Cranberry Bog This kind of wonder saved the bog for today and for to large multi-county organizations with portion of a property for conservation and Natural Resources belongs to fourth-graders.