Akkaneewut Jirapinyakul
Biographic Data
| ID | 4897328 |
|---|---|
| NAME | Akkaneewut Jirapinyakul |
| GIVEN NAMES | Akkaneewut |
| FAMILY NAME | Jirapinyakul |
| SIGNATURE | JIRAPINYAKUL A |
| AFFILIATIONS | Chulalongkorn University |
| ORCID | 0000-0002-1167-8912 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 1 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2023 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
Long-term vegetation dynamics, environmental changes, anthropogenic records, and carbon accumulation during 3,800 years in Krabi mangroves, Thailand
A multi-proxy paleoenvironmental study of the Khlong Thom mangroves in Krabi, Thailand reconstructed long-term vegetation and fire dynamics, sea-level changes, human impacts, and carbon accumulation rates over the past ca. 4,000 years. A period of marine dominance between 3,780 and 3,480 cal bp, characterised by Rhizophora dominance with increased carbon accumulation, coincided with a gradual sea-level decline following a mid-Holocene sea-level h…
East Asian monsoon- and Enso-regulated chemical weathering on North Thailand during the middle-late Holocene: Records from clay mineralogy and major element geochemistry in the Gulf of Thailand
Hydroclimate Variability in the Mainland Southeast Asia During the Last Glacial Maximum
The Last Glacial Maximum (LGM) is a key reference point for understanding past climate, but its complexity can lead to ambiguities in scope and interpretation. In this study, we applied a suite of geochemical techniques -XRF, grain size, and pollen analysis- to a well-dated sedimentary sequence from the lower central plain of Thailand. Our results show a gradual increase in fluvial runoff and precipitation from 26.5 to 24.6 cal ka BP, followed by…
Enso may have contributed to sea level changes in the Gulf of Thailand during the Late-Holocene
The Gulf of Thailand is ideal for studying eustatic sea level fluctuations in Southeast Asia due to its shallow basin and tectonic stability. However, our understanding of how this region’s relative sea level (RSL) has fluctuated over the Holocene epoch is far from complete. In this study, we used lithostratigraphy, loss on ignition, grain size, and pollen analyses to reconstruct the environmental changes in the Sam Roi Yot wetland, which was sig…
Enso may have contributed to sea level changes in the Gulf of Thailand during the Late-Holocene
The Gulf of Thailand is ideal for studying eustatic sea level fluctuations in Southeast Asia due to its shallow basin and tectonic stability. However, our understanding of how this region’s relative sea level (RSL) has fluctuated over the Holocene epoch is far from complete. In this study, we used lithostratigraphy, loss on ignition, grain size, and pollen analyses to reconstruct the environmental changes in the Sam Roi Yot wetland, which was sig…
Enso may have contributed to sea level changes in the Gulf of Thailand during the Late-Holocene
The Gulf of Thailand is ideal for studying eustatic sea level fluctuations in Southeast Asia due to its shallow basin and tectonic stability. However, our understanding of how this region’s relative sea level (RSL) has fluctuated over the Holocene epoch is far from complete. In this study, we used lithostratigraphy, loss on ignition, grain size, and pollen analyses to reconstruct the environmental changes in the Sam Roi Yot wetland, which was sig…
Hydroclimate Variability in the Mainland Southeast Asia During the Last Glacial Maximum
The Last Glacial Maximum (LGM) is a key reference point for understanding past climate, but its complexity can lead to ambiguities in scope and interpretation. In this study, we applied a suite of geochemical techniques -XRF, grain size, and pollen analysis- to a well-dated sedimentary sequence from the lower central plain of Thailand. Our results show a gradual increase in fluvial runoff and precipitation from 26.5 to 24.6 cal ka BP, followed by…
Long-term vegetation dynamics, environmental changes, anthropogenic records, and carbon accumulation during 3,800 years in Krabi mangroves, Thailand
A multi-proxy paleoenvironmental study of the Khlong Thom mangroves in Krabi, Thailand reconstructed long-term vegetation and fire dynamics, sea-level changes, human impacts, and carbon accumulation rates over the past ca. 4,000 years. A period of marine dominance between 3,780 and 3,480 cal bp, characterised by Rhizophora dominance with increased carbon accumulation, coincided with a gradual sea-level decline following a mid-Holocene sea-level h…
East Asian monsoon- and Enso-regulated chemical weathering on North Thailand during the middle-late Holocene: Records from clay mineralogy and major element geochemistry in the Gulf of Thailand
Geology and Paleoclimatology Research (4 works) · Climatology (2 works) · Geography (2 works) · Geology (2 works) · Paleontology (2 works) · Physical geography (2 works) · Ancient history (1 works) · Archaeology (1 works) · Charcoal (1 works) · Chemical composition (1 works)