Akkaneewut Chabangborn
Biographic Data
| ID | 6376173 |
|---|---|
| NAME | Akkaneewut Chabangborn |
| GIVEN NAMES | Akkaneewut |
| FAMILY NAME | Chabangborn |
| SIGNATURE | CHABANGBORN A |
| AFFILIATIONS | Chulalongkorn University |
| VERIFIED | No |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 26 |
| WORKS AS AUTHOR | 7 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2015 |
| LATEST PUBLICATION YEAR | 2020 |
| H-INDEX | 2 |
Environmental changes on the west coast of the Gulf of Thailand during the 8.2 ka event
Vegetation history and human impacts from Thong Pha Phum, western Thailand during the past 700 years
Implications for Provenance since the Last Glaciations in Southeastern Andaman Sea Sediments by Clay Mineralogy
This study presents high-resolution clay mineralogy of Core MASS-III-10, located in the southeastern Andaman Sea. The study aimed to investigate terrigenous sedimentary input from various potential provenances throughout different periods of geological time. The clay mineral assemblages of MASS-III-10 reveal a high amount of smectite at 73% (65-79%), a moderate kaolinite at 12% (10-17%), and a low illite and chlorite content(
Climate in Sundaland and Asian monsoon variability during the last deglaciation
Societal response to monsoonal fluctuations in NE Thailand during the demise of Angkor Civilisation
This paper investigates the possible social responses to changes in the strength of the southwest monsoon in northeastern Thailand during the currency of the Angkor civilisation. These assessments are based on hydrogen and carbon isotope records of leaf waxes (δD wax and δ 13 C wax ) from a 2000-year-long wetland sequence of Pa Kho in northeastern Thailand, a region that formed the northern boundary of the Angkor Kingdom. Our data indicate anthro…
Human adaptation to mid- to late-Holocene climate change in Northeast Thailand
This article integrates palaeoenvironmental and archaeological sequences covering the mid- to late-Holocene in Northeast Thailand. The former reveal the fluctuating intensity of the Asian summer monsoon, leading to periods of higher moisture availability with intervals of relative aridity. The latter are founded on a series of new radiocarbon determinations that provide a basic chronological framework, from the initial Neolithic settlements by ri…
Lake Kumphawapi revisited – The complex climatic and environmental record of a tropical wetland in NE Thailand
Kumphawapi, which is Thailand’s largest natural freshwater lake, contains a >10,000-year-long climatic and environmental archive. New data sets (stratigraphy, chronology, hydrogen isotopes, plant macrofossil and charcoal records) for two sedimentary sequences are here combined with earlier multi-proxy studies to provide a comprehensive reconstruction of past climatic and environmental changes for Northeast Thailand. Gradually higher moisture avai…
Human adaptation to mid- to late-Holocene climate change in Northeast Thailand
This article integrates palaeoenvironmental and archaeological sequences covering the mid- to late-Holocene in Northeast Thailand. The former reveal the fluctuating intensity of the Asian summer monsoon, leading to periods of higher moisture availability with intervals of relative aridity. The latter are founded on a series of new radiocarbon determinations that provide a basic chronological framework, from the initial Neolithic settlements by ri…
Societal response to monsoonal fluctuations in NE Thailand during the demise of Angkor Civilisation
This paper investigates the possible social responses to changes in the strength of the southwest monsoon in northeastern Thailand during the currency of the Angkor civilisation. These assessments are based on hydrogen and carbon isotope records of leaf waxes (δD wax and δ 13 C wax ) from a 2000-year-long wetland sequence of Pa Kho in northeastern Thailand, a region that formed the northern boundary of the Angkor Kingdom. Our data indicate anthro…
Lake Kumphawapi revisited – The complex climatic and environmental record of a tropical wetland in NE Thailand
Kumphawapi, which is Thailand’s largest natural freshwater lake, contains a >10,000-year-long climatic and environmental archive. New data sets (stratigraphy, chronology, hydrogen isotopes, plant macrofossil and charcoal records) for two sedimentary sequences are here combined with earlier multi-proxy studies to provide a comprehensive reconstruction of past climatic and environmental changes for Northeast Thailand. Gradually higher moisture avai…
Vegetation history and human impacts from Thong Pha Phum, western Thailand during the past 700 years
Lake Kumphawapi revisited – The complex climatic and environmental record of a tropical wetland in NE Thailand
Kumphawapi, which is Thailand’s largest natural freshwater lake, contains a >10,000-year-long climatic and environmental archive. New data sets (stratigraphy, chronology, hydrogen isotopes, plant macrofossil and charcoal records) for two sedimentary sequences are here combined with earlier multi-proxy studies to provide a comprehensive reconstruction of past climatic and environmental changes for Northeast Thailand. Gradually higher moisture avai…
Human adaptation to mid- to late-Holocene climate change in Northeast Thailand
This article integrates palaeoenvironmental and archaeological sequences covering the mid- to late-Holocene in Northeast Thailand. The former reveal the fluctuating intensity of the Asian summer monsoon, leading to periods of higher moisture availability with intervals of relative aridity. The latter are founded on a series of new radiocarbon determinations that provide a basic chronological framework, from the initial Neolithic settlements by ri…
Societal response to monsoonal fluctuations in NE Thailand during the demise of Angkor Civilisation
This paper investigates the possible social responses to changes in the strength of the southwest monsoon in northeastern Thailand during the currency of the Angkor civilisation. These assessments are based on hydrogen and carbon isotope records of leaf waxes (δD wax and δ 13 C wax ) from a 2000-year-long wetland sequence of Pa Kho in northeastern Thailand, a region that formed the northern boundary of the Angkor Kingdom. Our data indicate anthro…
Climate in Sundaland and Asian monsoon variability during the last deglaciation
Implications for Provenance since the Last Glaciations in Southeastern Andaman Sea Sediments by Clay Mineralogy
This study presents high-resolution clay mineralogy of Core MASS-III-10, located in the southeastern Andaman Sea. The study aimed to investigate terrigenous sedimentary input from various potential provenances throughout different periods of geological time. The clay mineral assemblages of MASS-III-10 reveal a high amount of smectite at 73% (65-79%), a moderate kaolinite at 12% (10-17%), and a low illite and chlorite content(
Environmental changes on the west coast of the Gulf of Thailand during the 8.2 ka event
Vegetation history and human impacts from Thong Pha Phum, western Thailand during the past 700 years
Geography (6 works) · Geology and Paleoclimatology Research (6 works) · Geology (5 works) · Physical geography (5 works) · Geological formations and processes (4 works) · Oceanography (4 works) · Archaeology and ancient environmental studies (3 works) · Climatology (3 works) · Ecology (3 works) · Monsoon (3 works)