Mangrove Ecology – Applications in Forestry and Costal Zone Management
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261 Comparative Morphology and Anatomy of Few Mangrove Species
261 International Journal of Bio-resource and Stress Management 2012, 3(1):001-017 Comparative Morphology and Anatomy of Few Mangrove Species in Sundarbans, West Bengal, India and its Adaptation to Saline Habitat Humberto Gonzalez Rodriguez1, Bholanath Mondal2, N. C. Sarkar3, A. Ramaswamy4, D. Rajkumar4 and R. K. Maiti4 1Facultad de Ciencias Forestales, Universidad Autonoma de Nuevo Leon, Carr. Nac. No. 85, Km 145, Linares, N.L. Mexico 2Department of Plant Protection, Palli Siksha Bhavana, Visva-Bharati, Sriniketan (731 236), West Bengal, India 3Department of Agronomy, SASRD, Nagaland University, Medziphema campus, Medziphema (PO), DImapur (797 106), India 4Vibha Seeds, Inspire, Plot#21, Sector 1, Huda Techno Enclave, High Tech City Road, Madhapur, Hyderabad, Andhra Pradesh (500 081), India Article History Abstract Manuscript No. 261 Mangroves cover large areas of shoreline in the tropics and subtropics where they Received in 30th January, 2012 are important components in the productivity and integrity of their ecosystems. High Received in revised form 9th February, 2012 variability is observed among the families of mangroves. Structural adaptations include Accepted in final form th4 March, 2012 pneumatophores, thick leaves, aerenhyma in root helps in surviving under flooded saline conditions. There is major inter- and intraspecific variability among mangroves. In this paper described morpho-anatomical characters helps in identification of family Correspondence to and genus and species of mangroves. Most of the genus have special type of roots which include Support roots of Rhizophora, Pnematophores of Avicennia, Sonneratia, Knee *E-mail: [email protected] roots of Bruguiera, Ceriops, Buttress roots of Xylocarpus. Morpho-anatomically the leaves show xerophytic characteristics. -
Section 1-Maggie-Final AM
KEY TO GROUP 1 Mangroves and plants of saline habitats, i.e., regularly inundated by king tides. A. leaves B. leaves C. simple D. compound opposite alternate leaf leaf 1 Mature plants less than 60 cm high, often prostrate and succulent go to 2 1* Mature plants greater than 60 cm high, shrubs or trees go to 4 2 Plants without obvious leaves, succulent (samphires) go to Group 1.A 2* Plants with obvious leaves, sometimes succulent go to 3 3 Grass, non-succulent, leaves narrow, margins rolled inwards go to Group 1.B 3* Plants with succulent leaves, may be flattened, cylindrical or almost so go to Group 1.C 4 Trees or shrubs with opposite leaves (see sketch A) go to 5 4* Trees or shrubs with alternate leaves (B) go to 6 5 Leaves with oil glands visible when held to the light and an aromatic smell when crushed or undersurface whitish go to Group 1.D Large oil glands as seen with a good hand lens 5* Leaves without oil glands or a whitish undersurface, but prop roots, knee roots or buttresses may be present go to Group 1.E 6 Plants with copious milky sap present when parts, such as stems and leaves are broken (CAUTION) go to Group 1.F 6* Plants lacking milky sap when stems or leaves broken go to 7 7 Shrubs or trees with simple leaves (C) go to Group 1.G 7* Trees with compound leaves (D) go to Group 1.H 17 GROUP 1.A Plants succulent with no obvious leaves (samphires). -
Saltmarsh and Samphire
Baker, J. L. (2015) Marine Assets of Yorke Peninsula. Volume 2 of report for Natural Resources - Northern and Yorke, South Australia 6. Saltmarsh and Samphire © A. Brown Figure 6.1: Saltmarsh with samphire, in NY NRM Region. (A) Point Davenport; (B) Winninowie Conservation Park. Photos (c) A. Brown. (B): (c) Google Earth. Asset Saltmarsh and Samphire Description Areas of saline, mineral-rich, organic-rich, and low oxygen coastal soils within and above high tide level, often fronted by mangroves, and backed by saltbush shrubland. Saltmarsh supports various salt-tolerant plants, with samphires being the most common and significant in terms of cover in South Australia. There are distinct assemblages of salt-tolerant invertebrates associated with saltmarsh habitats. Saltmarshes provide habitat for fishes, including juveniles of species which utilise other marine habitats, and are an important feeding area for various bird species, including migratory shore birds. Examples of Birds Main Species Cormorant species (e.g.; Pied, Little Pied, and Black-faced) Caspian Tern and Little Tern Pied Oystercatcher and Sooty Oystercatcher Black-winged Stilt, Banded Stilt, Great Egret, White-faced Heron, Little Egret the threatened species Hooded Plover Little Stint Red-capped Plover Slender-billed Thornbill (Samphire Thornbill) Rock Parrot The raptors Eastern Osprey and White-bellied Sea Eagle Migratory shorebirds listed under international treaties, such as Bar-tailed Godwit, Curlew Sandpiper and Sharp-tailed Sandpiper, Red-necked Stint, Grey Plover , Red Knot, Common Greenshank, Ruddy Turnstones Bony Fishes juvenile Yelloweye Mullet juvenile Greenback Flounder juvenile Southern Blue-spotted Flathead Western Striped Grunter Congolli Glass Goby Small-mouthed Hardyhead Silver Fish Smooth Toadfish Goby species such as Blue-spotted Goby and Southern Longfin Goby Adelaide Weedfish Baker, J. -
Impacts of Climate Change on Australian Marine Life Part C
Impacts of Climate Change on Australian Marine Life Part C: Literature Review Editors: Alistair J. Hobday, Thomas A. Okey, Elvira S. Poloczanska, Thomas J. Kunz, Anthony J. Richardson CSIRO Marine and Atmospheric Research report to the Australian Greenhouse Office , Department of the Environment and Heritage September 2006 Published by the Australian Greenhouse Office, in the Department of the Environment and Heritage ISBN: 978-1-921297-07-6 © Commonwealth of Australia 2006 This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without prior written permission from the Commonwealth, available from the Department of the Environment and Heritage. Requests and inquiries concerning reproduction and rights should be addressed to: Assistant Secretary Land Management and Science Branch Department of the Environment and Heritage GPO Box 787 CANBERRA ACT 2601 This report is in 3 parts: Part A. Executive Summary Part B. Technical Report Part C. Literature Review Please cite this report section as: Hobday, A.J., Okey, T.A., Poloczanska, E.S., Kunz, T.J. & Richardson, A.J. (eds) 2006. Impacts of climate change on Australian marine life: Part C. Literature Review. Report to the Australian Greenhouse Office, Canberra, Australia. September 2006. Disclaimer The views and opinions expressed in this publication are those of the authors and do not necessarily reflect those of the Australian Government or the Minister for the Environment and Heritage. While reasonable efforts have been made to ensure that the contents of this publication are factually correct, the Commonwealth does not accept responsibility for the accuracy or completeness of the contents, and shall not be liable for any loss or damage that may be occasioned directly or indirectly through the use of, or reliance on, the contents of this publication. -
Species Composition and Zonal Distribution of Mangrove Plants in the Myeik Coastal Areas of Myanmar
Journal of Aquaculture & Marine Biology Research Article Open Access Species composition and zonal distribution of mangrove plants in the Myeik coastal areas of Myanmar Abstract Volume 9 Issue 2 - 2020 The species composition and zonal distribution of mangroves in five research sites viz., Tin-Zar-Ni-Win,1 U Soe-Win2 Kapa, Masanpa, Panadoung, Kywe Ka Yan and Kyauk Phyar from Myeik coastal areas 1Marine Biologist, Fauna & Flora International (FFI), Myanmar were studied from December 2017 to July 2018. Transect lines in landward, seaward 2Department of Marine Science, Mawlamyine University, and shoreline, and plots based on Point Center Quarter Method (PCQM) were used. Myanmar A total of 21 species of true mangrove were recorded. Rhizophora apiculata and R. Mucronata were the most dominant species in the study sites, especially in the seaward Correspondence: Tin-Zar-Ni-Win, Marine Biologist, Fauna & areas. Among the recorded species, Aegiceras corniculatum, Avicennia officinalis, R. Flora International (FFI), Myanmar apiculata, R. mucronata, Sonneratia alba and Nypa fruticans were distributed in all study Email sites. Bruguiera gymnorhiza and B.cylindrica, were recorded only in shoreline areas and Heritiera littoralisis was found only in landward areas in all study sites. Among the Received: April 07, 2020 | Published: April 28, 2020 study sites, Kapa has been designated as the highest species composition, representing 17 species, whereas Kyauk Phyar, representing 12 species as the lowest species composition. The environmental parameters of mangrove forests were also provided in all study sites. The various salinity and temperature ranges of seawater (25.0-30.0‰ and 28.0-32.0ºC) and soil (25.0-33.0‰ and 27.6-31.4ºC) significantly controlled the distribution of mangrove species of mangroves. -
DMAAC – February 1973
LUNAR TOPOGRAPHIC ORTHOPHOTOMAP (LTO) AND LUNAR ORTHOPHOTMAP (LO) SERIES (Published by DMATC) Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Scale: 1:250,000 Projection: Transverse Mercator Sheet Size: 25.5”x 26.5” The Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Series are the first comprehensive and continuous mapping to be accomplished from Apollo Mission 15-17 mapping photographs. This series is also the first major effort to apply recent advances in orthophotography to lunar mapping. Presently developed maps of this series were designed to support initial lunar scientific investigations primarily employing results of Apollo Mission 15-17 data. Individual maps of this series cover 4 degrees of lunar latitude and 5 degrees of lunar longitude consisting of 1/16 of the area of a 1:1,000,000 scale Lunar Astronautical Chart (LAC) (Section 4.2.1). Their apha-numeric identification (example – LTO38B1) consists of the designator LTO for topographic orthophoto editions or LO for orthophoto editions followed by the LAC number in which they fall, followed by an A, B, C or D designator defining the pertinent LAC quadrant and a 1, 2, 3, or 4 designator defining the specific sub-quadrant actually covered. The following designation (250) identifies the sheets as being at 1:250,000 scale. The LTO editions display 100-meter contours, 50-meter supplemental contours and spot elevations in a red overprint to the base, which is lithographed in black and white. LO editions are identical except that all relief information is omitted and selenographic graticule is restricted to border ticks, presenting an umencumbered view of lunar features imaged by the photographic base. -
Four Marine Digenean Parasites of Austrolittorina Spp. (Gastropoda: Littorinidae) in New Zealand: Morphological and Molecular Data
Syst Parasitol (2014) 89:133–152 DOI 10.1007/s11230-014-9515-2 Four marine digenean parasites of Austrolittorina spp. (Gastropoda: Littorinidae) in New Zealand: morphological and molecular data Katie O’Dwyer • Isabel Blasco-Costa • Robert Poulin • Anna Falty´nkova´ Received: 1 July 2014 / Accepted: 4 August 2014 Ó Springer Science+Business Media Dordrecht 2014 Abstract Littorinid snails are one particular group obtained. Phylogenetic analyses were carried out at of gastropods identified as important intermediate the superfamily level and along with the morpholog- hosts for a wide range of digenean parasite species, at ical data were used to infer the generic affiliation of least throughout the Northern Hemisphere. However the species. nothing is known of trematode species infecting these snails in the Southern Hemisphere. This study is the first attempt at cataloguing the digenean parasites Introduction infecting littorinids in New Zealand. Examination of over 5,000 individuals of two species of the genus Digenean trematode parasites typically infect a Austrolittorina Rosewater, A. cincta Quoy & Gaim- gastropod as the first intermediate host in their ard and A. antipodum Philippi, from intertidal rocky complex life-cycles. They are common in the marine shores, revealed infections with four digenean species environment, particularly in the intertidal zone representative of a diverse range of families: Philo- (Mouritsen & Poulin, 2002). One abundant group of phthalmidae Looss, 1899, Notocotylidae Lu¨he, 1909, gastropods in the marine intertidal environment is the Renicolidae Dollfus, 1939 and Microphallidae Ward, littorinids (i.e. periwinkles), which are characteristic 1901. This paper provides detailed morphological organisms of the high intertidal or littoral zone and descriptions of the cercariae and intramolluscan have a global distribution (Davies & Williams, 1998). -
Mangroves and Saltmarshes of Moreton Bay
https://moretonbayfoundation.org/ 1 Moreton Bay Quandamooka & Catchment: Past, present, and future Chapter 5 Habitats, Biodiversity and Ecosystem Function Mangroves and saltmarshes of Moreton Bay Abstract The mangroves and saltmarshes of Moreton Bay comprising 18,400 ha are important habitats for biodiversity and providing ecosystem services. Government policy and legislation largely reflects their importance with protection provided through a range of federal and state laws, including the listing of saltmarsh communities in 2013 under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act). Local communities also conserve and manage mangroves and saltmarshes. Recent scientific research on these ecosystems in Moreton Bay has described food webs, habitat use by fauna, carbon sequestration and effects of climate change. The area of saltmarsh has declined by 64% since 1955 due to mangrove encroachment into saltmarsh habitats and past conversion to rural and urban land uses. Mangrove encroachment into saltmarsh habitats, which has been reported in other locations in Australia and across the world, has increased the area of mangrove habitat by 6.4% over the same period. This is consistent with predictions of habitat changes under climate change, and demonstrates the need for management strategies that ensure these ecosystems are maintained. Keywords: coastal wetlands, intertidal, wetland management, EPBC Act, wetland change, drivers of wetland change, South East Queensland, soil carbon stocks Introduction Mangroves and saltmarshes, which are components of the estuarine wetlands of Moreton Bay, are dominated by salt-tolerant vegetation that occurs from approximately mean sea level to the highest astronomical tidal plane. They occur within the river systems and tidal creeks of Moreton Bay as well as on the comparatively open coasts of the Bay where they fringe both islands and the mainland. -
Phylogeny and Evolution of Lepidoptera
EN62CH15-Mitter ARI 5 November 2016 12:1 I Review in Advance first posted online V E W E on November 16, 2016. (Changes may R S still occur before final publication online and in print.) I E N C N A D V A Phylogeny and Evolution of Lepidoptera Charles Mitter,1,∗ Donald R. Davis,2 and Michael P. Cummings3 1Department of Entomology, University of Maryland, College Park, Maryland 20742; email: [email protected] 2Department of Entomology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560 3Laboratory of Molecular Evolution, Center for Bioinformatics and Computational Biology, University of Maryland, College Park, Maryland 20742 Annu. Rev. Entomol. 2017. 62:265–83 Keywords Annu. Rev. Entomol. 2017.62. Downloaded from www.annualreviews.org The Annual Review of Entomology is online at Hexapoda, insect, systematics, classification, butterfly, moth, molecular ento.annualreviews.org systematics This article’s doi: Access provided by University of Maryland - College Park on 11/20/16. For personal use only. 10.1146/annurev-ento-031616-035125 Abstract Copyright c 2017 by Annual Reviews. Until recently, deep-level phylogeny in Lepidoptera, the largest single ra- All rights reserved diation of plant-feeding insects, was very poorly understood. Over the past ∗ Corresponding author two decades, building on a preceding era of morphological cladistic stud- ies, molecular data have yielded robust initial estimates of relationships both within and among the ∼43 superfamilies, with unsolved problems now yield- ing to much larger data sets from high-throughput sequencing. Here we summarize progress on lepidopteran phylogeny since 1975, emphasizing the superfamily level, and discuss some resulting advances in our understanding of lepidopteran evolution. -
The Saltwater Crocodile, Crocodylus Porosus Schneider, 1801, in the Kimberley Coastal Region
Journal of the Royal Society of Western Australia, 94: 407–416, 2011 The Saltwater Crocodile, Crocodylus porosus Schneider, 1801, in the Kimberley coastal region V Semeniuk1, C Manolis2, G J W Webb2,4 & P R Mawson3 1 V & C Semeniuk Research Group 21 Glenmere Rd., Warwick, WA 6024 2 Wildlife Management International Pty. Limited PO Box 530, Karama, NT 0812 3 Department of Environment & Conservation Locked Bag 104, Bentley D.C., WA 6983 4 School of Environmental Research, Charles Darwin University, NT 0909 Manuscript received April 2011; accepted April 2011 Abstract The Australian Saltwater Crocodile, Crocodylus porosus, is an iconic species of the Kimberley region of Western Australia. Biogeographically, it is distributed in the Indo-Pacific region and extends to northern Australia, with Australia representing the southernmost range of the species. In Western Australia C. porosus now extends to Exmouth Gulf. In the Kimberley region, C. porosus is found in most of the major river systems and coastal waterways, with the largest populations in the rivers draining into Cambridge Gulf, and the Prince Regent and Roe River systems. The Kimberly region presents a number of coastlines to the Saltwater Crocodile. In the Cambridge Gulf and King Sound, there are mangrove-fringed or mangrove inhabited tidal flats and tidal creeks, that pass landwards into savannah flats, providing crocodiles with a landscape and seascape for feeding, basking and nesting. The Kimberley Coast is dominantly rocky coasts, rocky ravines/ embayments, sediment-filled valleys with mangroves and tidal creeks, that generally do not pass into savannah flats, and areas for nesting are limited. Since the 1970s when the species was protected, the depleted C. -
Kimberley Marine Biota. History and Environment
RECORDS OF THE WESTERN AUSTRALIAN MUSEUM 84 001–018 (2014) DOI: 10.18195/issn.0313-122x.84.2014.001-018 SUPPLEMENT Kimberley marine biota. History and environment Barry Wilson Research Associate, Department of Aquatic Zoology, Western Australian Museum, Locked Bag 49, Welshpool DC, Western Australia 6986, Australia. Email: [email protected] ABSTRACT – The remote tropical Kimberley region of Western Australia is introduced, its physical marine environment, habitats and classifi cation into bioregions are described, and its marine science history is summarised. An introduction to the ongoing Western Australian Museum marine biological survey program and its objectives are also provided. The geology, metocean conditions and climate of the region are summarised. A primary division of the Kimberley coastline is noted with a northern section dominated by Proterozoic meta-sedimentary and igneous rocks (Kimberley and Bonaparte Gulf Bioregions) and a southern section dominated by Mesozoic and Cainozoic sedimentary rocks (King Sound and Canning Bioregions). In the former section inner shelf seabed sediments overlying the inundated Yampi Plateau are principally of terrestrial origin while in the Canning Bioregion they are principally marine carbonates. On the middle and outer shelf (Oceanic Shoals and North West Shelf Bioregions) sediments are primarily marine carbonates. Along the shelf margin the water is clear and oligotrophic and subject to the Indonesian Through Flow current that originates in the western Pacifi c. The coastal zone is macrotidal, currents are predominantly tide driven and the coastal water is turbid and probably nutrient rich. These environmental differences and the different connectivity regimes account for distinctive offshore and coastal reef communities. KEYWORDS: marine flora, marine fauna, habitats, geology, ocean currents, climate, species distributions, biogeographic affi nities, IMCRA Bioregions, science history INTRODUCTION traditional lands in their care under the Healthy The Kimberley is the northernmost part Country program. -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei