Citation
Kamaludin Hassan, . (2005) Peat: its significance as climate record. [Proceedings Paper]
Abstract
Peat is formed by the accumulation of decayed plant matter in naturally low oxygen and highly acidic areas. Throughout the geological past it is known that peat had been accumulating on and off. The interrupted accumulations reflect the prevailing surrounding environmental changes that had affected the nature of peat formation. The record from our region and its interpretation is here discussed and deliberated.
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Abstract
Peat is formed by the accumulation of decayed plant matter in naturally low oxygen and highly acidic areas. Throughout the geological past it is known that peat had been accumulating on and off. The interrupted accumulations reflect the prevailing surrounding environmental changes that had affected the nature of peat formation. The record from our region and its interpretation is here discussed and deliberated.
Additional Metadata
Item Type: | Proceedings Paper |
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Additional Information: | 8 refs. |
AGROVOC Term: | PEATLANDS |
AGROVOC Term: | SWAMPS |
AGROVOC Term: | WETLANDS |
AGROVOC Term: | GEOMORPHOLOGY |
AGROVOC Term: | PEAT SOILS |
AGROVOC Term: | MALAYSIA |
Geographical Term: | MALAYSIA |
Depositing User: | Ms. Norfaezah Khomsan |
Last Modified: | 24 Apr 2025 05:28 |
URI: | http://webagris.upm.edu.my/id/eprint/16788 |
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