Skip to content

Rates and Drivers of Mangrove Deforestation in Southeast Asia, 2000-2012

The mangrove forests of Southeast Asia are highly biodiverse and provide multiple ecosystem services upon which millions of people depend. Mangroves enhance fisheries and coastal protection, and store among the highest densities of carbon of any ecosystem globally. Mangrove forests have experienced extensive deforestation owing to global demand for commodities, and previous studies have identified the expansion of aquaculture as largely responsible. The proportional conversion of mangroves to different land use types has not been systematically quantified across Southeast Asia, however, particularly in recent years. In this study, the authors apply a combined geographic information system and remote sensing method to quantify the key proximate drivers (i.e., replacement land uses) of mangrove deforestation in Southeast Asia between 2000 and 2012.

Data Resources (1)

Data Resource Preview - Rates and drivers of mangrove deforestation in Southeast Asia, 2000-2012

Additional Info

Field Value
စာတမ်းအမျိုးအစား Reports, journal articles, and research papers (including theses and dissertations)
စာရွက်စာတမ်း၏ ဘာသာစကား
  • အင်္ဂလိပ်ဘာသာစကား
ခေါင်းစဉ်များ
  • Deforestation drivers
  • Fish farming and aquaculture
  • Forest policy and administration
  • Sustainable use forest
ပထဝီဧရိယာ (spatial range)
  • အင်ဒိုနီးရှား
  • မြန်မာ
  • ထိုင််း
မူပိုင်ခွင့် Yes
ရယူခြင်းနှင့် အသုံးပြုခြင်း အကန့်အသတ်များ

Copyright & Usage: http://www.pnas.org/preview_site/misc/userlicense.xhtml

ပြင်ဆင်ချက် 1
ခွင့်ပြုချက် unspecified
ဆက်သွယ်ရန်

To whom correspondence should be addressed: Email: d.r.richards@nus.edu.sg.

ရေးသားသူ (တစ်ဦးချင်း) Daniel R. Richards
ပူးတွဲရေးသားသူ (တစ်ဦးချင်းစီ) Daniel A. Friess
ISSN နံပါတ် 1091-6490
ထုတ်ဝေသူ National Academy of Sciences
ထုတ်ဝေသည့်ရက်စွဲ 2016
စာမျက်နှာခွဲ 6
အဓိကစကားလုံးများ forest loss,aquaculture,oil palm,indonesia
တင်ခဲ့သည့်ရက်စွဲ ဖေဖော်ဝါရီ 12, 2018, 17:50 (UTC)
ပြန်လည်ပြင်ဆင်သည့်ရက်စွဲ ဖေဖော်ဝါရီ 12, 2018, 18:15 (UTC)