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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. -
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IN THE NAME OF GOD IRAN NAMA RAILWAY TOURISM GUIDE OF IRAN List of Content Preamble ....................................................................... 6 History ............................................................................. 7 Tehran Station ................................................................ 8 Tehran - Mashhad Route .............................................. 12 IRAN NRAILWAYAMA TOURISM GUIDE OF IRAN Tehran - Jolfa Route ..................................................... 32 Collection and Edition: Public Relations (RAI) Tourism Content Collection: Abdollah Abbaszadeh Design and Graphics: Reza Hozzar Moghaddam Photos: Siamak Iman Pour, Benyamin Tehran - Bandarabbas Route 48 Khodadadi, Hatef Homaei, Saeed Mahmoodi Aznaveh, javad Najaf ...................................... Alizadeh, Caspian Makak, Ocean Zakarian, Davood Vakilzadeh, Arash Simaei, Abbas Jafari, Mohammadreza Baharnaz, Homayoun Amir yeganeh, Kianush Jafari Producer: Public Relations (RAI) Tehran - Goragn Route 64 Translation: Seyed Ebrahim Fazli Zenooz - ................................................ International Affairs Bureau (RAI) Address: Public Relations, Central Building of Railways, Africa Blvd., Argentina Sq., Tehran- Iran. www.rai.ir Tehran - Shiraz Route................................................... 80 First Edition January 2016 All rights reserved. Tehran - Khorramshahr Route .................................... 96 Tehran - Kerman Route .............................................114 Islamic Republic of Iran The Railways -
(Euphorbiaceae) in Iran with the Description of Euphorbia Mazandaranica Sp
Nordic Journal of Botany 32: 257–278, 2014 doi: 10.1111/njb.01690 © 2014 Th e Authors. Nordic Journal of Botany © 2014 Nordic Society Oikos Subject Editor: Arne Strid. Accepted 26 July 2012 Synopsis of Euphorbia subgen. Esula sect. Helioscopia (Euphorbiaceae) in Iran with the description of Euphorbia mazandaranica sp. nov. Amir Hossein Pahlevani and Ricarda Riina A. H. Pahlevani ([email protected]), Dept of Botany, Iranian Research Inst. of Plant Protection, PO Box 1454, IR-19395 Tehran, Iran. AHP also at: Dept of Plant Systematics, Univ. of Bayreuth, DE-95440 Bayreuth, Germany. – R. Riina, Real Jardin Bot á nico, RJB-CSIC, Plaza Murillo 2, ES-28014 Madrid, Spain. Euphorbia subgen. Esula with about 480 species is one of the most diverse and complex lineages of the giant genus Euphorbia . Species of this subgenus are usually herbaceous and are mainly distributed in temperate areas of the Northern Hemisphere. Th is paper updates the taxonomy and distribution of Euphorbia (subgen. Esula ) sect. Helioscopia in Iran since the publication of ‘ Flora Iranica ’ in 1964. We provide a key, species descriptions, illustrations (for most species), distribution maps, brief characterization of ecology as well as relevant notes for the 12 species of this section occurring in Iran. As a result of this revision, E. altissima var. altissima is reported as new for the country, and a new species from northern Iran, Euphorbia mazandaranica , is described and illustrated. With the exception of E. helioscopia , a widespread weed in temperate regions worldwide, the remaining species occur in the Alborz, Zagros and northwestern regions of Iran. Euphorbia L. -
Effects of Climate Change on Forested Wetland Soils [Chapter 9]
CHAPTER Effects of climate change on forested wetland soils 9 Carl C. Trettina,*, Martin F. Jurgensenb, Zhaohua Daia aSouthern Research Station, USDA Forest Service, Cordesville, SC, United States, bSchool of Forest Resources and Environmental Science, Michigan Technological University, Houghton, MI, United States *Corresponding author ABSTRACT Wetlands are characterized by water at or near the soil surface for all or significant part of the year, are a source for food, fiber and water to society, and because of their position in landscapes and ecological structure help to moderate floods. They are also unique ecosystems with long-persistent flora and fauna. Because water is a driving factor for existence as a wetland, these systems are particularly vulnerable to climate change, especially as warming is accompanied by changes the quality and quantity of water moving through these systems. Because they are such diverse ecosystems, wetlands respond differently to stressors and, therefore, require different management and restoration techniques. In this chapter we consider forested wetland soils, their soil types, functions, and associated responses to climate change. Wetland processes are not well understood and therefore additional information is needed on these areas. In addition, more knowledge is needed on the interface between wetlands, uplands, and tidal waters. Introduction Wetlands are defined on the basis of saturated anaerobic soil conditions near the surface during the growing season and plants that are adapted to growing in anoxic soils (Cowardin et al., 1979). While specific definitions of wetlands vary by country or region, it is the presence of saturated soils and hydrophytic trees and understory plants that differentiate forested wetlands from upland forests. -
Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト
Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト ● Asia 4 Bangladesh 7 China アジア バングラデシュ 中国 1 Afghanistan 9 Khulna 6 Hangzhou アフガニスタン クルナ 杭州(ハンチォウ) 1 Herat 10 Kotwalipara 7 Wuhan ヘラート コタリパラ 武漢(ウハン) 2 Kabul 11 Meherpur 8 Cyprus カブール メヘルプール キプロス 3 Nili 12 Moulvibazar 1 Aglantzia ニリ モウロビバザール アグランツィア 2 Armenia 13 Narayanganj 2 Ammochostos (Famagusta) アルメニア ナラヤンガンジ アモコストス(ファマグスタ) 1 Yerevan 14 Narsingdi 3 Kyrenia エレバン ナールシンジ キレニア 3 Azerbaijan 15 Noapara 4 Kythrea アゼルバイジャン ノアパラ キシレア 1 Agdam 16 Patuakhali 5 Morphou アグダム(県) パトゥアカリ モルフー 2 Fuzuli 17 Rajshahi 9 Georgia フュズリ(県) ラージシャヒ ジョージア 3 Gubadli 18 Rangpur 1 Kutaisi クバドリ(県) ラングプール クタイシ 4 Jabrail Region 19 Swarupkati 2 Tbilisi ジャブライル(県) サルプカティ トビリシ 5 Kalbajar 20 Sylhet 10 India カルバジャル(県) シルヘット インド 6 Khocali 21 Tangail 1 Ahmedabad ホジャリ(県) タンガイル アーメダバード 7 Khojavend 22 Tongi 2 Bhopal ホジャヴェンド(県) トンギ ボパール 8 Lachin 5 Bhutan 3 Chandernagore ラチン(県) ブータン チャンダルナゴール 9 Shusha Region 1 Thimphu 4 Chandigarh シュシャ(県) ティンプー チャンディーガル 10 Zangilan Region 6 Cambodia 5 Chennai ザンギラン(県) カンボジア チェンナイ 4 Bangladesh 1 Ba Phnom 6 Cochin バングラデシュ バプノム コーチ(コーチン) 1 Bera 2 Phnom Penh 7 Delhi ベラ プノンペン デリー 2 Chapai Nawabganj 3 Siem Reap Province 8 Imphal チャパイ・ナワブガンジ シェムリアップ州 インパール 3 Chittagong 7 China 9 Kolkata チッタゴン 中国 コルカタ 4 Comilla 1 Beijing 10 Lucknow コミラ 北京(ペイチン) ラクノウ 5 Cox's Bazar 2 Chengdu 11 Mallappuzhassery コックスバザール 成都(チォントゥ) マラパザーサリー 6 Dhaka 3 Chongqing 12 Meerut ダッカ 重慶(チョンチン) メーラト 7 Gazipur 4 Dalian 13 Mumbai (Bombay) ガジプール 大連(タァリィェン) ムンバイ(旧ボンベイ) 8 Gopalpur 5 Fuzhou 14 Nagpur ゴパルプール 福州(フゥチォウ) ナーグプル 1/108 Pages -
A-414 History of Tropical Peatland in Southeast Asia
15TH INTERNATIONAL PEAT CONGRESS 2016 Abstract No: A-414 HISTORY OF TROPICAL PEATLAND IN SOUTHEAST ASIA Furukawa Hisao Kyoto University, Japan * Corresponding author: [email protected] SUMMARY Geohistory of tropical peatlands in Southeast Asia and a historical retrospect of the exploitation are presented. Keywords: Age, stratigraphy, early and modern ways of exploitation. INTRODUCTION Coastal plains of the Malay Peninsula, Sumatra and Borneo bordering the Sunda Sea were, and still are partly, the realm of swamp forests which included mangrove at seaward outskirts, freshwater swamp forests in the tidal zone, and peat swamp forests inland. Under natural conditions, the ground surface is covered by tropical woody peat layers of varying thickness. These peatlands emerged through the Holocene submersion of the vast and flat terrains at the periphery of the former Sunda Land, and the productive tropical rain forests which expanded over the region. The tropical peatlands inhabited only by mammals, apes, birds and reptiles, remained miasmic for long periods against human interferences because of dense forests, high humidity, numberless mosquitoes, often submerged and bumpy ground surface. Now amidst the worldwide industrialism, they are swiftly changing into one of the important agro-industrial bases, and no one cannot deny that industrialism is a powerful engine to make a people richer and more free. On the other hand, we have seen negative effects of industrialism so often. London was famous for its smog by the mid 20th century. Japan in the 1960s to 1970s was an emporium with so many kinds of environmental pollution and induced diseases. These issues were met, and even now are met through dialogs, scientific studies and legislative measures supported by our own accord. -
Tropical Wetlands and Redd+: Three Unique Scientific Challenges for Policy
TROPICAL WETLANDS AND REDD+: THREE UNIQUE SCIENTIFIC CHALLENGES FOR POLICY Daniel A Friess1 Assoc Professor Department of Geography, National University of Singapore. The carbon sequestration and storage value of terrestrial habitats is now increasingly appreciated, and is the basis for Payment for Ecosystem Service (PES) policies such as REDD+. Tropical wetlands may be suitable for inclusion in such schemes because of the disproportionately large volume of carbon they are able to store. However, tropical wetlands offer a number of unique challenges for carbon management and policy compared to terrestrial forest systems: 1) Tropical wet- lands are dynamic and subject to a wide range of physical and ecological processes that affect their long-term carbon storage potential – thus, such systems can quickly become a carbon source instead of a sink; 2) Carbon dynamics in tropical wetlands often operate over longer timescales than are currently covered by REDD+ payments; and 3) Much of the carbon in a tropical wetland is stored in the soil, so monitoring, reporting and verification (MRV) needs to adequately encapsu- late the entire ecosystem and not just the vegetative component. This paper discusses these physical and biological concepts, and highlights key legal, man- agement and policy questions that must be considered when constructing a policy framework to conserve these crucial ecosystems. Introduction Tropical wetlands (primarily mangroves and peat swamp forests) provide a multitude of important ecosys- tem services such as coastal protection, pollutant assimilation, water retention and flood alleviation, nutrient production, and support of offshore fisheries and livelihoods.2 Tropical wetlands are also carbon rich; mangroves, for example, can contain four to six times as much carbon as other terrestrial forest types,3 and peat swamps accumulate extensive carbon stores in large peat domes that have formed over thousands of years. -
An Overview on the Basis of Urban Planning and Social Life of Safavid Cities
Intl. J. Humanities (2016) Vol. 23 (3): (1-13) An Overview on the basis of Urban Planning and Social Life of Safavid Cities Abed Taghavi 1, Hassan Hashemi Zarjabad 2, Maryam Asgari Veshareh 3 Received: 2016/3/2 Accepted: 2016/10/11 Abstract In the Safavid era, cities played a decisive role in the activities of urban social life, especially with regard to commodity, distribution and exchanging system between urban and rural society as well as defining the role of organizations in the commercial process. This paper is based on historical analyzing method where the authors could utilize primary sources to study social and economic states of urban life in Persian cities during Safavid. Farah Abad, Isfahan and Bandar Abbas in North, Center and South of Iran have been examined. These cities were selected considering their functional nature as producer, industrial (processor) and exporter centers. The outcome of the study shows that the cities founded and developed during Safavid, specially on Silk Road, during the reign of Shah Abbas I (996- 1038 AH), played the role of producer, distributer and exporter in north, center and south of Iran. Based on their functional capacities, cities of that era are divided into three types: producer of raw materials, intermediary and processing, and finally exporter (port) cities. The analysis of economic relations of those cities indicates that the king had despotic monopolization of all aspects of the cities where the urban economy deeply on agricultural economy of countryside. Keywords: Islamic Cites; Financial Relations; Safavid Era; Silk Route; Economic unction. Downloaded from eijh.modares.ac.ir at 20:19 IRST on Tuesday September 28th 2021 1.Assistant Professor of Archaeology, University of Mazandaran, [email protected] 2. -
Tropical Peatlands of Southeast Asia
Tropical peatlands of Southeast Asia: Functions, threats and the role of fire in climate change mitigation Matthew Warren [email protected] USDA Forest Service, Northern Research Station Tropical peat swamp forests are ecologically diverse Tropical wetland forests Structurally similar to other upland tropical wet forests. Hydric conditions drive ecosystem processes and functions, supporting unique biological communities physically and physiologically adapted to the anaerobic soil environment. Southeast Asia: The global center of tropical peatlands About 44.1 Mha of tropical peatlands ~11% of the total peatland area; volume is ~18 -25% (Page et al. 2011). About 25 Mha (56%) of tropical peatlands occur in SE Asia. Indonesia contains around 47% (Page et al. 2011). TRUE EXTENT? Miettinen et al. 2011 Posa et al. (2011) Extensive peatlands occur in Sumatra, Borneo, and W. Papua (not shown) Posa et al. 2011 Ecosystem Services Environmental functions that support human well-being - Supporting: Primary production, nutrient cycling, soil maintenance - Provisioning: Food, water, fiber, timber, fuel, medicine, NTFP’s - Regulating: Climate, floods, sedimentation, drought, disease - Cultural: Aesthetic, spiritual, recreational, educational, ecotourism - Biological: Unique biodiversity, genetic and biochemical resources Hydrological Regulation Faiz Rahman $ustenance Timber • Local construction • Commercial extraction • Fuel wood • Charcoal Biological Diversity Many flagship species for conservation find refuge in wetland forests. Countless plants, fungi, fish and insects remain poorly known or undescribed. B. Kauffman ZSL- Berbak Orangutan Tropical Peatland Project: www.outrop.com Carbon Storage • Tropical wetlands store more C per ha than any other tropical forest type • Tropical peatlands store about 88.6 Gt C, 15-19% of global peat C pool • Estimates range from about 2000-3000 Mg C/ha, average 2009 MgC/ha globally (Page et al. -
Agroclimatic Zones Map of Iran Explanatory Notes
AGROCLIMATIC ZONES MAP OF IRAN EXPLANATORY NOTES E. De Pauw1, A. Ghaffari2, V. Ghasemi3 1 Agroclimatologist/ Research Project Manager, International Center for Agricultural Research in the Dry Areas (ICARDA), Aleppo Syria 2 Director-General, Drylands Agricultural Research Institute (DARI), Maragheh, Iran 3 Head of GIS/RS Department, Soil and Water Research Institute (SWRI), Tehran, Iran INTRODUCTION The agroclimatic zones map of Iran has been produced to as one of the outputs of the joint DARI-ICARDA project “Agroecological Zoning of Iran”. The objective of this project is to develop an agroecological zones framework for targeting germplasm to specific environments, formulating land use and land management recommendations, and assisting development planning. In view of the very diverse climates in this part of Iran, an agroclimatic zones map is of vital importance to achieve this objective. METHODOLOGY Spatial interpolation A database was established of point climatic data covering monthly averages of precipitation and temperature for the main stations in Iran, covering the period 1973-1998 (Appendix 1, Tables 2-3). These quality-controlled data were obtained from the Organization of Meteorology, based in Tehran. From Iran 126 stations were accepted with a precipitation record length of at least 20 years, and 590 stations with a temperature record length of at least 5 years. The database also included some precipitation and temperature data from neighboring countries, leading to a total database of 244 precipitation stations and 627 temperature stations. The ‘thin-plate smoothing spline’ method of Hutchinson (1995), as implemented in the ANUSPLIN software (Hutchinson, 2000), was used to convert this point database into ‘climate surfaces’. -
Effects of Peat Swamp Logging and Agricultural Expansion on Species Richness of Native Mammals in Peninsular Malaysia
Accepted Manuscript Title: Effects of peat swamp logging and agricultural expansion on species richness of native mammals in Peninsular Malaysia Authors: Nurfatin Adila, Selvadurai Sasidhran, Norizah Kamarudin, Chong Leong Puan, Badrul Azhar, David B. Lindenmayer PII: S1439-1791(16)30197-9 DOI: http://dx.doi.org/doi:10.1016/j.baae.2017.04.002 Reference: BAAE 51028 To appear in: Received date: 23-10-2016 Accepted date: 4-4-2017 Please cite this article as: {http://dx.doi.org/ This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Effects of peat swamp logging and agricultural expansion on species richness of native mammals in Peninsular Malaysia Nurfatin Adila1, Selvadurai Sasidhran1,2, Norizah Kamarudin1, Chong Leong Puan1, Badrul Azhar1,3, David B. Lindenmayer4 1Department of Forest Management, Faculty of Forestry, Universiti Putra Malaysia, 43400 Serdang, Selangor, Malaysia 2WWF Malaysia, 1 Jalan PJS 5/28A, Petaling Jaya Commercial Centre (PJCC), 46150 Petaling Jaya, Selangor, Malaysia 3Biodiversity Unit, Institute of Bioscience, Universiti Putra Malaysia, 43400 Serdang, Selangor, Malaysia 4The Fenner School of Environment and Society, ANU College of Medicine, Biology and Environment, Australian National University, Canberra ACT 0200, Australia Corresponding author. E-mail address: [email protected] (B. -
Riparian Wetlands of Tropical Streams
Riparian Wetlands of Tropical Streams Karl M. Wantzen, Catherine M. Yule, Klement Tockner, and Wolfgang J. Junk I. Introduction 199 II. Types of Riparian Wetlands 201 III. Hydrology 206 IV. Biodiversity 208 V. Aquatic-Terrestrial Linkages 209 VI. Human Impacts, Conservation, and Sustainable Management 211 VII. Conclusions and Prospects 212 References 213 Riparian wetlands are temporarily or permanently inundated and/or water-logged zones along the margins of streams and rivers. They link permanent aquatic habitats with upland terrestrial habitats, and surface-water with groundwater. This chapter focuses on riparian wetlands associated with low-order tropical streams, which have been lesser studied than equivalent ecotones associated with large rivers. We demonstrate that (a) these wetlands provide valuable habitats for diverse and highly specialized flora and fauna; (b) these serve as important longitudinal and transversal corridors for exchange of material and dispersal of biota; and (c) these perform important ecosystem functions locally as well as at the catchment scale. For example, headwater wetlands are key sites for mutual subsidies between terrestrial and aquatic systems, and are pivotal areas for the transformation of nutrients and organic matter. All riparian wetlands are subject to significant modification by humans, which compromises their functional integrity. However, riparian ecotones along low- order streams often occupy limited areas beyond the banks, and awareness of their ecological importance is limited in comparison to the extensive wetlands and floodplains associated with large lowland rivers. Creating awareness of the need for their sustainable management will be a challenging task. I. INTRODUCTION Riparian wetlands have been defined as ‘lowland terrestrial ecotones which derive their high water tables and alluvial soils from drainage and erosion of adjacent uplands on the one side or from periodic flooding from the other’ (McCormick, 1979).