Eco-System Development

Total Page:16

File Type:pdf, Size:1020Kb

Eco-System Development Last Update: 6 December 2017 Part – II ECOSYSTEM DEVELOPMENT E.T - 1 It is also called ecological succession. When a new area is destroyed by some disturbances. After sometime plants appear in these area. At 1st step some algae, lichen, fungi occur then moss & fern herbs & grasses shrubs Tress. She area again covered by vegetation & animals also occurs in the area. So, a bare area courted into a stable ecosystem. In doing so, the ecosystem passes from an initial less complex stage to a mature or more complex stage i.e. at 1st biodiversity is low & then final stage. Initial stage of succession is called pioneer stage and final stage is called climax stage and inter mediate stages are known as shrubs stage. Pioneer stage Seralstage climax stage Ecosystem tends towards maturity and in doing so it passes from less complex pioneer stage to more stable state which is climax stage. There is a progressive change but not unidirectional change. Definition :- Ecological succession is a directional progressive change in which there is an orderly replacement of one community and in doing so it passes from a simple pioneer stage to a complex & stable climax stage through several intermediate seral stage. However, Margalef (1968) prefers to replace the term climax by term more mature ecosystem. In our biosphere most mature ecosystem are replacement by coral reef, tropical rain forest etc. So, coral reef & tropical rain forest is the e.g. of most mature eco-system. During eco-system various factors are involve these are biotic factor, climatic factor, physiographic factor & geologic factor. These influence the development of ecosystem. Classification of Succession :- 1) Depending upon the role played by above these factor or pre dominant factor succession may be classified- a) Biosere b) Cliosere c) Eosere d) Geosere a) Biosere :- If biotic factors are predominating in succession, i.e. organisms are responsible. b) Cliosere :- When climate is primarily responsible for bringing about succession. c) Eosere :- If physiogeographic factors are primarily responsible (i.e.- topograph). d) Geosere :- If geological properties of earth are primarily bringing about the succession. If geological properties of earth are primarily bringing about the succession. Last 3 type succession (cliosere, eosere, geosere) are called palaeoeology because these 3 requires considerable time (involves 100,000 years) for succession. Biosere involve less period of time. Here biotic factor is more important. e.g.- Land dure appears by mud 2) Depending upon their origin succession can be classified a) Hydrosere b) Halosere c) Xerosere a) Hydrosere :- If a succession is start from a fresh water body, that type of succession is called Hydrosere. b) Halosere :- When succession is start from a salt marsh that type of succession is called Halosere. c) Xerosere :- When succession start from rock, soil, that type of succession is called Xerosere. 3) Now have few other kinds of succession. It can classified- a) Primary & secondary succession. b) Autotrophic & heterotrophic succession. c) Autogenic & allogenic succession. - 1 - d) Unidirectional & cyclic succession. a) Primary & secondary succession :- Primary succession are those succession which takes place in area devoid of organism or which not previously occupy by organism and environment is predominantly inorganic in nature. Here no living thing and have no organic matter. e.g. – Newly exposed sand dune, recent lava flow. b) Secondary succession :- Secondary succession is the succession which takes in environment and which previously occupied by living thing or organic matter. e.g.- In deforested area, In harvested crop land. Slash & burn cultivation is called shifting cultivation. Autotrophic succession :- Autotrophic succession which is characterized by early & continued dominance P of autotrophic elements. In this succession community metabolism is autotrophic in nature. i.e. 1 R P = Community production. R = Community respiration. Environment is inorganic in nature. e.g.- Autotrophs succession i.e. plant succession. Heterotrophic Succession :- In this, succession is characterized by early and continued predominance of heterotrophic elements. It is predominantly inorganic in nature. Heterotrophic succession follows Autotrophic community metabolism is heterotrophic in nature. i.e. - e.g. – Fungi Autogenic Succession :- In this succession internal forces is involved. It is self driven succession. Environmental changes are brought about by biotic factor. Causal factors are located within the succession decomposition takes place. Allogenic succession :- Allogenic successions are those succession in which factors are located outside the environment (i.e.- climate physiochemical properties of soil, light, rainfall, temperature). So, these allogenic factors cause allogenic succession. Initial phase is allogenic & latter phase is autogenic succession. Unidirectional & cyclic succession :- Most of the successions are unidirectional. 1st pioneer change & then climax change through seral stage. But sometime it cyclically repeated. e.g.- There are some shallow which is seasonal in nature that means every year it is drying & with it. So, its all organism also die and after rain alive from pioneer stage it starts succession. This is the cyclic succession. Example of Succession Heterotrophic Succession :- Major Community situated in some minor community. These minor Community provided substratum for their own type of succession. These substratum are predominantly organic in nature. So, it is heterotrophic in nature. Such succession is characterized by early and continued dominance of heterotrophic elements. Therefore these serve as an excellent example of heterotrophic succession. It was studied by Winston (1956). He studied the succession in a fallen Acron in the forest field. It is Oat like fruit & the shell is hard. Succession in Acron is start when it hangs from a tree & fruit is invaded by ‘Acron weevil’ (curculio rectus). The adult female burrows through the surface of the Acron and lays egg inside the fruit (endosperm). From the egg larva hatches out & it starts feeding on the embryo. Sometimes though happens that some pathogenic hole which has been created by Acron weevil & they also start consuming the embryo. It pathogenic fungi like Penicillium & Fusarium. They destroy the embryo which is brown in color. And such larva of weevil become stunted in growth. This feature represent the pioneer stage. These group Of feature are followed by another group Of feature. These are fungivores and scavengers and include cheese mite and Acron moth (Velentinia glandenella). Cheese mite belonging to family. Tryophagus & Phyzoglypheus. These are fungivores in nature. Acron moth belonging to Velentinia glandenella. It lay egg in the surface of the Acron or in the exit hole - 2 - created by curculso rectus. The larva of Velentinia after entering through the exit hole turns round and spins a tough web to seal the exit hole. Cheese mites are consuming the remainder of endosperm and also feeds on the faces of the previous occupants (Curculso rectus). So, the pioneer stage is replaced by second group or organisms. What happens? The acron is attacked by cellulose and liguine consuming fungi which mostly attacked the surface of the Acron and then invade inside also. These are another group Of organism. These are followed by fungivores mites of the soil & collembola. They will feed on the cellulose & liguine consuming fungi & the surface of acron. These are followed by predatory mites belonging to genus gamasellus. They invade acron be cause they are extremely flattened mite & enter through cracks and crevices. They consuming fungivores and predatory mites. So, invaded group Of organisms are replaced by another group Gradually replaced. Ultimately outer surface be comes very thin large amount of soil enter into the cavity and Acron collapsed and then it is invaded by generalized soil fauna e.g.- Centriped, milliped, etc. so, there represents the final stage. This type of succession occur in an environment which is predominantly characterized by early & continued predominance of heterotrophs. So, this is an e.g. of heterotrophic succession. Fundamental aspects of Succession :- 1) There is an orderly and directed change of both environment and community. Both undergo continuous reciprocal influence and adjustment. 2) Change in environment is brought about by organisms themselves. So, it is an e.g. of autotrophic succession. 3) Exploitation of the environment makes the habitat unfavourable for the survival of pioneer organism and instead create a favourable environment from other group of organisms. 4) Kinds of animals and plants change continuously during such process. 5) Since supply of sp is limited. Therefore succession can not go no for ever. As such succession is an asymmetric process. 6) Succession calumniates (stop) with the establishment of relatively stable ecosystem. 7) The ecological succession is community control. The physical environment determines the pattern of succession but does not cause it. It is caused by the biotic factor. It is a community control phenomenon. 8) Time require for succession depends on geography, climate, substrate, other physical factor and species Involved. Trends of Autogenic succession :- Basic ecology by Odum (1983). A) Energetics :- 1) Biomass & organic detritus increase. 2) Gross production in primary production. 3) Net production decrease. 4) Respiration increase. P 5) Production/respiration i.e. ratio
Recommended publications
  • Environmental Science (Ce-101) Unit- I
    Lecture Notes of Environmental Science ENVIRONMENTAL SCIENCE (CE-101) UNIT- I Introduction to Environmental Science: The science of Environment studies is a multi-disciplinary science because it comprises various branches of studies like chemistry, physics, medical science, life science, agriculture, public health, sanitary engineering etc. It is the science of physical phenomena in the environment. It studies of the sources, reactions, transport, effect and fate of physical a biological species in the air, water and soil and the effect of from human activity upon these. Environment – The word environment comes from the greek word “environner” meaning surroundings around us. Scope of Environmental studies: The environment consists of four segments as under: 1. Atmosphere: The atmosphere implies the protective blanket of gases, surrounding the earth: It sustains life on the earth. It saves it from the hostile environment of outer space. It absorbs most of the cosmic rays from outer space and a major portion of the electromagnetic radiation from the sun. It transmits only here ultraviolet, visible, near infrared radiation (300 to 2500 nm) and radio waves. (0.14 to 40 m) while filtering out tissue-damaging ultraviolet waves below about 300 nm. The atmosphere is composed of nitrogen and oxygen. Besides, argon, carbon dioxide, and trace gases. 2. Hydrosphere: The Hydrosphere comprises all types of water resources oceans, seas, lakes, rivers, streams, reservoir, polar icecaps, glaciers, and groundwater. Nature 97% of the earth’s water supply is in the oceans, Prepared by: Er. Arshad Abbas Deptt. of Civil Engg. KMCUAF University Lucknow About 2% of the water resources are locked in the polar icecaps and glaciers.
    [Show full text]
  • The Bodwad Sarvajanik Co-Op.Education Society Ltd., Bodwad Arts, Commerce and Science College, Bodawd Question Bank Class :-S.Y
    The Bodwad Sarvajanik Co-Op.Education Society Ltd., Bodwad Arts, Commerce and Science College, Bodawd Question Bank Class :-S.Y.B.Sc SEM:- IV Subject: - BOTANY- 402 Plant Ecology 1. The science which deals with relationship between organisms and their environment is called a) Morphology b) Palynology c) Taxonomy d) Ecology 2. The meaning of Greek word Oikas a) Nature b) Environment c) House d) Temple 3. The term ecology coined by a) Odum b) Tansley c) Haeckel d) None 4. Autecology deals with the study of a) Ecology of individual species b) Ecology of many species c) Ecology of community d) All of these 5. Synecology deals with the study of a) Ecology of individual species b) Ecology of many species c) Ecology of community d) All of these 6. The branch of ecology which deals with the study of the organisms and geological environments of past is called a) Cytoecology b) Palecology c) Synecology d) Autoecology 7. Ecology deals with the study of a) Living beings b) Living and non living components c) Reciprocal relationship between living and non living components d) Biotic and Abiotic components 8. Phylloclade is modified a) Root b) Leaf c) Stem d) Bud 9. Cuscuta is a) Parasite b) Epiphyte c) Symbiont d) Lichen 10. Mycorrhiza is example of a) Symbiotic relationship b) Parasitic relationship c) Saprophytic relationship d) Negative interaction 11. Edaphic ecological factors are concerned with a) Rainfall b) Light c) Competition d) Soil 12. The soil is said to be physiologically dry when a) Temperature band light available to plants is insufficient b) There is abundance of water in soil c) Soil water is with high concentration of salts d) Both b and c 13.
    [Show full text]
  • Birds of the Nova Scotia— New Brunswick Border Region by George F
    Birds of the Nova Scotia— New Brunswick border region by George F. Boyer Occasional Paper Number 8 Second edition Canadian Wildlife Service Environment Canada Environnement Canada Wildlife Service Service de la Faune Birds of the Nova Scotia - New Brunswick border region by George F. Boyer With addendum by A. J. Erskine and A. D. Smith Canadian Wildlife Service Occasional Paper Number 8 Second edition Issued under the authority of the Honourable Jack Davis, PC, MP Minister of the Environment John S. Tener, Director Canadian Wildlife Service 5 Information Canada, Ottawa, 1972 Catalogue No. CW69-1/8 First edition 1966 Design: Gottschalk-)-Ash Ltd. 4 George Boyer banding a barn swallow in June 1952. The author George Boyer was born in Woodstock, New Brunswick, on August 24, 1916. He graduated in Forestry from the University of New Brunswick in 1938 and served with the Canadian Army from 1939 to 1945. He joined the Canadian Wildlife Service in 1947, and worked out of the Sackville office until 1956. During that time he obtained an M.S. in zoology from the University of Illinois. He car­ ried on private research from April 1956 until July 1957, when he rejoined CWS. He worked out of Maple, Ontario, until his death, while on a field trip near Aultsville. While at Sackville, Mr. Boyer worked chiefly on waterfowl of the Nova Scotia-New Brunswick border region, with special emphasis on Pintails and Black Ducks. He also studied merganser- salmon interrelationships on the Miramichi River system, Woodcock, and the effects on bird popu­ lations of spruce budworm control spraying in the Upsalquitch area.
    [Show full text]
  • Effects of Age on Hummock Succession in Bogs
    Effects of age on hummock succession in bogs By Joel Vallier Abstract Ecological succession is the change in communities over time. We chose to study the successional stages of hummocks in a bog using age. We hypothesized that hummock plant richness should increase then decrease with age because of successional flora species mixing. We also hypothesized that hummock density, and hummock size will increase with age. Our study site was a bog at Mud Lake located in Cheboygan County, Michigan. We set up two 100 meter transects, divided them into zones based on age then recorded hummock surface area and hummock density. Plant richness was also recorded. There was a significant difference in plant richness with hummock age but only when surface area was used a covariant. Surface area was not significantly different among different aged zones. Hummock density did not have any correlation with age. Places were successional flora species mixed provided more plant richness and also showed trends of higher surface area. The tree line altered our results in the youngest zones because it had late successional species mixed with early successional species. This gave one of our youngest zones the highest plant richness. This shows that trends exist between hummock size, and plant richness but the surrounding morphology has a large impact. Introduction Succession within an ecological community is the change in species composition over time. This can change the biodiversity of the environment by altering conditions making it more adaptable by other species (Katz, 1926). This can be seen in the classic hydrosere succession model, where infilling of a shallow lake by sediments produces a sequential trend of vegetation communities staring with marsh shrub and moss species and ending with climax forests composed mostly of woody species (Klinger, 1996).
    [Show full text]
  • Chapter 5: Vegetation of Sphagnum-Dominated Peatlands
    CHAPTER 5: VEGETATION OF SPHAGNUM-DOMINATED PEATLANDS As discussed in the previous chapters, peatland ecosystems have unique chemical, physical, and biological properties that have given rise to equally unique plant communities. As indicated in Chapter 1, extensive literature exists on the classification, description, and ecology of peatland ecosystems in Europe, the northeastern United States, Canada, and the Rocky Mountains. In addition to the references cited in Chapter 1, there is some other relatively recent literature on peatlands (Verhoeven 1992; Heinselman 1963, 1970; Chadde et al., 1998). Except for efforts on the classification and ecology of peatlands in British Columbia by the National Wetlands Working Group (1988), the Burns Bog Ecosystem Review (Hebda et al. 2000), and the preliminary classification of native, low elevation, freshwater vegetation in western Washington (Kunze 1994), scant information exists on peatlands within the more temperate lowland or maritime climates of the Pacific Northwest (Oregon, Washington, and British Columbia). 5.1 Introduction There are a number of classification schemes and many different peatland types, but most use vegetation in addition to hydrology, chemistry and topological characteristics to differentiate among peatlands. The subject of this report are acidic peatlands that support acidophilic (acid-loving) and xerophytic vegetation, such as Sphagnum mosses and ericaceous shrubs. Ecosystems in Washington state appear to represent a mosaic of vegetation communities at various stages of succession and are herein referred to collectively as Sphagnum-dominated peatlands. Although there has been some recognition of the unique ecological and societal values of peatlands in Washington, a statewide classification scheme has not been formally adopted or widely recognized in the scientific community.
    [Show full text]
  • Environmental Science in the Course of Different Levels
    THIS PAGE IS BLANK NEW AGE INTERNATIONAL (P) LIMITED, PUBLISHERS New Delhi · Bangalore · Chennai · Cochin · Guwahati · Hyderabad Jalandhar · Kolkata · Lucknow · Mumbai · Ranchi PUBLISHING FOR ONE WORLD Visit us at www.newagepublishers.com Copyright © 2006 New Age International (P) Ltd., Publishers Published by New Age International (P) Ltd., Publishers All rights reserved. No part of this ebook may be reproduced in any form, by photostat, microfilm, xerography, or any other means, or incorporated into any information retrieval system, electronic or mechanical, without the written permission of the publisher. All inquiries should be emailed to [email protected] ISBN (10) : 81-224-2330-2 ISBN (13) : 978-81-224-2330-3 PUBLISHING FOR ONE WORLD NEW AGE INTERNATIONAL (P) LIMITED, PUBLISHERS 4835/24, Ansari Road, Daryaganj, New Delhi - 110002 Visit us at www.newagepublishers.com Education is a process of development which includes the three major activities, teaching, training and instruction. Teaching is social as well as a professional activity. It is science as well as art. Modern education is not in a sphere but it has a long and large area of study. Now a days most part of the world population is facing different problems related with the nature and they are studying the solutions to save the nature and global problems, but on the second hand we even today do not try to understand our local problems related to the nature. So for the awareness of the problems of P nature and pollution the higher education commission has suggested to add the Environmental Science in the course of different levels.
    [Show full text]
  • ENVIRONMENTAL SYSTEMS and SOCIETIES SL IB Academy Environmental Systems and Societies Study Guide
    STUDY GUIDE ENVIRONMENTAL SYSTEMS AND SOCIETIES SL www.ib.academy IB Academy Environmental systems and societies Study Guide Available on learn.ib.academy Author: Laurence Gibbons Design Typesetting This work may be shared digitally and in printed form, but it may not be changed and then redistributed in any form. Copyright © 2020, IB Academy Version: ESS.2.1.200320 This work is published under the Creative Commons BY-NC-ND 4.0 International License. To view a copy of this license, visit creativecommons.org/licenses/by-nc-nd/4.0 This work may not used for commercial purposes other than by IB Academy, or parties directly licenced by IB Academy. If you acquired this guide by paying for it, or if you have received this guide as part of a paid service or product, directly or indirectly, we kindly ask that you contact us immediately. Laan van Puntenburg 2a ib.academy 3511ER, Utrecht [email protected] The Netherlands +31 (0) 30 4300 430 0 Welcome to the IB Academy guide book for IB Environmental Systems and Society Standard Level. This guide contains all the theory you should know for your final exam. To achieve top marks this theory should be complimented with case studies. Although not covered in this booklet, we provide some in our online podcast series. The guide starts with an explanation of systems and models which are the foundations for the whole course. We will then look at systems in the natural world before turning our attention to humans and their impact. Throughout the guide there are helpful hints from the former IB students who now teach with IB Academy.
    [Show full text]
  • Compiled and Circulated by Dr. Poulami Adhikary Mukherjee, Assistant Professor, Department of Zoology, Narajole Raj College
    COMPILED AND CIRCULATED BY DR. POULAMI ADHIKARY MUKHERJEE, ASSISTANT PROFESSOR, DEPARTMENT OF ZOOLOGY, NARAJOLE RAJ COLLEGE SSoommee CCoommmmuunniittyy CChhaarraacctteerriissttiicc TTeerrmmiinnoollooggyy BBYY DDRR.. PPOOUULLAAMMII AADDHHIIKKAARRYY MMUUKKHHEERRJJEEEE AASSSSIISSTTAANNTT PPRROOFFEESSSSOORR DDEEPPAARRTTMMEENNTT OOFF ZZOOOOLLOOGGYY NNAARRAAJJOOLLEE RRAAJJ CCOOLLLLEEGGEE ZOOLOGY: SEM- I, PAPER- C2T: ECOLOGY, UNIT 3: COMMUNITY COMPILED AND CIRCULATED BY DR. POULAMI ADHIKARY MUKHERJEE, ASSISTANT PROFESSOR, DEPARTMENT OF ZOOLOGY, NARAJOLE RAJ COLLEGE Vertical Stratification: Stratification in the field of ecology refers to the vertical layering of a habitat; the arrangement of vegetation in layers. It classifies the layers (sing. stratum, pl. strata) of vegetation largely according to the different heights to which their plants grow. The individual layers are inhabited by different animal and plant communities (stratozones). The vertical distribution of different species occupying different levels in an ecosystem is called stratification. Trees occupy the topmost vertical layer of a forest, shrubs occupy ZOOLOGY: SEM- I, PAPER- C2T: ECOLOGY, UNIT 3: COMMUNITY COMPILED AND CIRCULATED BY DR. POULAMI ADHIKARY MUKHERJEE, ASSISTANT PROFESSOR, DEPARTMENT OF ZOOLOGY, NARAJOLE RAJ COLLEGE the second layer, and herbs and grasses occupy the bottommost or base layers. Vertical structure in terrestrial plant habitats: The following layers are generally distinguished: forest floor (root and moss layers), herb, shrub, understory and canopy layers. These vegetation layers are primarily determined by the height of their individual plants, the different elements may however have a range of heights. The actual layer is characterised by the height ZOOLOGY: SEM- I, PAPER- C2T: ECOLOGY, UNIT 3: COMMUNITY COMPILED AND CIRCULATED BY DR. POULAMI ADHIKARY MUKHERJEE, ASSISTANT PROFESSOR, DEPARTMENT OF ZOOLOGY, NARAJOLE RAJ COLLEGE range in which the vast majority of photosynthetic organs (predominantly leaves) are found.
    [Show full text]
  • New Records of the Diatoms (Bacillariophyceae) from the Coastal Lagoons in Korea
    Journal of Marine Science and Engineering Article New Records of the Diatoms (Bacillariophyceae) from the Coastal Lagoons in Korea Daeryul Kwon 1 , Mirye Park 1 , Chang Soo Lee 1, Chaehong Park 2 and Sang Deuk Lee 3,* 1 Protist Research Team, Microbial Research Department, Nakdonggang National Institute of Biological Resources (NNIBR), 137, Donam 2-gil, Sangju-si 37182, Korea; [email protected] (D.K.); [email protected] (M.P.); [email protected] (C.S.L.) 2 Human and Eco-Care Center, Konkuk University, Seoul 05029, Korea; [email protected] 3 Bioresources Collection & Research Team, Bioresources Collection & Bioinformation Department, Nakdonggang National Institute of Biological Resources (NNIBR), 137, Donam 2-gil, Sangju-si 37182, Korea * Correspondence: [email protected]; Tel.: +82-54-530-0898; Fax: +82-54-530-0899 Abstract: Lagoons are natural bodies of water that are isolated from the sea due to the develop- ment of a sand bar or spit. Each lagoon has distinct ecological characteristics, and these sites also serve as popular tourist attractions because they are common habitats for migratory birds and are characterized by beautiful natural scenery. Lagoons also have distinct ecological characteristics from those of their associated estuaries, and there are active research efforts to classify, qualify, and quantify the high biodiversity of lagoons. The lagoons in Korea are primarily distributed in the East Sea, and are represented by Hwajinpo, Yeongrangho, and Gyeongpoho. Here, we report the discovery of 11 unrecorded diatom species (Diploneis didyma, Mastogloia elliptica, Cosmioneis citriformis, Haslea crucigera, Pinnularia bertrandii, Pinnularia nodosa var. percapitata, Gyrosigma sinense, Gomphonema guaraniarum, Gomphonema italicum, Navicula freesei, Trybionella littoralis var.
    [Show full text]
  • The Mangal of Sinai: Limits of an Ecosystem
    Helgoi~nder wiss. Meeresunters. 30, 295-314 (1977) The mangal of Sinai: Limits of an ecosystem F. D. PoR 1, I. DOR 2 & A. AMIR 2 1 Department of Zoology, The Hebrew University of Jerusalem; Jerusalem, Israel, and 2 Oceanography Program, The Hebrew University of Jerusalem; Jerusalem, Israel ABSTRACT: The northernmost mangrove forests of the Red Sea are described. Temperature and salinity conditions were found to be extreme, obviously reducing the diversity of the ecosystem and presumably setting the geographical limits of its distribution. The Sinai mangal grows on hard fossil coral bottom, without any influence of estuarine sedimentation. Primary production of the open Red Sea waters is extremely low, therefore, the rich biomass of the Sinai mangal is built up by an autarkic nutrient recycling system. Several biotic zones within the Sinai mangal are described following an inshore-offshore transect. Vertical zonation of algae and animals on the aerial roots of Avicennia is discussed. The Sinai mangal, "Shura" by its local name, is proposed as an ideal model for the study of trophic relations within the mangrove biome. INTRODUCTION The mangrove forests or "mangal" (MacNae, 1968) are a typical life community of the tropical shores. Although equal in importance to coral reefs, as far as fre- quency is concerned, mangrove forests have been little studied as integral ecosystems. Much has been written about the phytosociology of the mangrove trees, but studies including also algal and animal associates are rare (Walsh, 1974). The Sinai mangrove was first mentioned by Ascherson (1887) and the mangroves of the Egyptian African coast by Kassas & Zahran (i967).
    [Show full text]
  • The Key to Keyhaven
    KS4 Geography 111112 Ecosystems Route: Lymington-Yarmouth The Key to Keyhaven STUDENT INTRODUCTION The picture above shows Keyhaven Saltmarshes, which are part of the more extensive salt marsh system which extends along the coast to the east of Lymington. In this resource you are going to learn all about what slat marshes are and how they develop. On your ferry crossing, from Lymington to Yarmouth (or vice versa), you will be able to see the salt marshes for yourself. You will also be learning about their importance, threats to salt marsh ecosystems and what can be done to manage them. What you learn may form part of a case study for your exam, so make sure you pay attention. Introducing Salt Marshes PRE-VISIT Read the following information very carefully – you will then complete a TASKS series of tasks based on what you have read and learnt! Salt marshes are found in coastal environments where sheltered water allows sediment to be deposited and build up over time to create a unique ecosystem. Sheltered water is found behind a spit, and this can provide the perfect conditions for deposition of sediment. Similarly, estuaries, where rivers enter the sea, are areas where large accumulations of sediment which have been carried down by the river can be deposited. Where they develop at river mouths, the water will be brackish – partly salty and partly fresh water). Sediment is deposited and initially builds up to form mud flats. These are exactly what the name suggests – flat areas of mud! They are what is known as intertidal, in that they are covered at high tide and exposed at low tide.
    [Show full text]
  • Glossary of Landscape and Vegetation Ecology for Alaska
    U. S. Department of the Interior BLM-Alaska Technical Report to Bureau of Land Management BLM/AK/TR-84/1 O December' 1984 reprinted October.·2001 Alaska State Office 222 West 7th Avenue, #13 Anchorage, Alaska 99513 Glossary of Landscape and Vegetation Ecology for Alaska Herman W. Gabriel and Stephen S. Talbot The Authors HERMAN w. GABRIEL is an ecologist with the USDI Bureau of Land Management, Alaska State Office in Anchorage, Alaskao He holds a B.S. degree from Virginia Polytechnic Institute and a Ph.D from the University of Montanao From 1956 to 1961 he was a forest inventory specialist with the USDA Forest Service, Intermountain Regiono In 1966-67 he served as an inventory expert with UN-FAO in Ecuador. Dra Gabriel moved to Alaska in 1971 where his interest in the description and classification of vegetation has continued. STEPHEN Sa TALBOT was, when work began on this glossary, an ecologist with the USDI Bureau of Land Management, Alaska State Office. He holds a B.A. degree from Bates College, an M.Ao from the University of Massachusetts, and a Ph.D from the University of Alberta. His experience with northern vegetation includes three years as a research scientist with the Canadian Forestry Service in the Northwest Territories before moving to Alaska in 1978 as a botanist with the U.S. Army Corps of Engineers. or. Talbot is now a general biologist with the USDI Fish and Wildlife Service, Refuge Division, Anchorage, where he is conducting baseline studies of the vegetation of national wildlife refuges. ' . Glossary of Landscape and Vegetation Ecology for Alaska Herman W.
    [Show full text]