Abstract
The Southeast Asian mainland is located in the central path of the Asian summer monsoon, a region where paleoclimatic data are still sparse. Here we present a multi-proxy (TOC, C/N, δ13C, biogenic silica, and XRF elemental data) study of a 1.5m sediment/peat sequence from Lake Pa Kho, northeast Thailand, which is supported by 20 AMS 14C ages. Hydroclimatic reconstructions for Pa Kho suggest a strengthened summer monsoon between BC 170-AD 370, AD 800-960, and after AD 1450; and a weakening of the summer monsoon between AD 370-800, and AD 1300-1450. Increased run-off and a higher nutrient supply after AD 1700 can be linked to agricultural intensification and land-use changes in the region. This study fills an important gap in data coverage with respect to summer monsoon variability over Southeast Asia during the past 2000 years and enables the mean position of the Intertropical Convergence Zone (ITCZ) to be inferred based on comparisons with other regional studies. Intervals of strengthened/weaker summer monsoon rainfall suggest that the mean position of the ITCZ was located as far north as 35°N between BC 170-AD 370 and AD 800-960, whereas it likely did not reach above 17°N during the drought intervals of AD 370-800 and AD 1300-1450. The spatial pattern of rainfall variation seems to have changed after AD 1450, when the inferred moisture history for Pa Kho indicates a more southerly location of the mean position of the summer ITCZ.
| Language | English |
|---|---|
| Pages | 62-71 |
| Number of pages | 10 |
| Journal | Quaternary Science Reviews |
| Volume | 111 |
| Early online date | 02 Feb 2015 |
| DOIs | |
| Publication status | Published - 01 Mar 2015 |
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Keywords
- Asian monsoon
- Geochemistry
- Last two millennia
- Paleoclimate
- Wetland/peatland
Cite this
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Hydroclimatic shifts in northeast Thailand during the last two millennia - the record of Lake Pa Kho. / Chawchai, Sakonvan; Chabangborn, Akkaneewut; Fritz, Sherilyn; Väliranta, Minna; Mörth, Carl-Magnus; Blaauw, Maarten; Reimer, Paula J.; Krusic, Paul J.; Löwemark, Ludvig; Wohlfarth, Barbara.
In: Quaternary Science Reviews, Vol. 111, 01.03.2015, p. 62-71.Research output: Contribution to journal › Article
TY - JOUR
T1 - Hydroclimatic shifts in northeast Thailand during the last two millennia - the record of Lake Pa Kho
AU - Chawchai, Sakonvan
AU - Chabangborn, Akkaneewut
AU - Fritz, Sherilyn
AU - Väliranta, Minna
AU - Mörth, Carl-Magnus
AU - Blaauw, Maarten
AU - Reimer, Paula J.
AU - Krusic, Paul J.
AU - Löwemark, Ludvig
AU - Wohlfarth, Barbara
PY - 2015/3/1
Y1 - 2015/3/1
N2 - The Southeast Asian mainland is located in the central path of the Asian summer monsoon, a region where paleoclimatic data are still sparse. Here we present a multi-proxy (TOC, C/N, δ13C, biogenic silica, and XRF elemental data) study of a 1.5m sediment/peat sequence from Lake Pa Kho, northeast Thailand, which is supported by 20 AMS 14C ages. Hydroclimatic reconstructions for Pa Kho suggest a strengthened summer monsoon between BC 170-AD 370, AD 800-960, and after AD 1450; and a weakening of the summer monsoon between AD 370-800, and AD 1300-1450. Increased run-off and a higher nutrient supply after AD 1700 can be linked to agricultural intensification and land-use changes in the region. This study fills an important gap in data coverage with respect to summer monsoon variability over Southeast Asia during the past 2000 years and enables the mean position of the Intertropical Convergence Zone (ITCZ) to be inferred based on comparisons with other regional studies. Intervals of strengthened/weaker summer monsoon rainfall suggest that the mean position of the ITCZ was located as far north as 35°N between BC 170-AD 370 and AD 800-960, whereas it likely did not reach above 17°N during the drought intervals of AD 370-800 and AD 1300-1450. The spatial pattern of rainfall variation seems to have changed after AD 1450, when the inferred moisture history for Pa Kho indicates a more southerly location of the mean position of the summer ITCZ.
AB - The Southeast Asian mainland is located in the central path of the Asian summer monsoon, a region where paleoclimatic data are still sparse. Here we present a multi-proxy (TOC, C/N, δ13C, biogenic silica, and XRF elemental data) study of a 1.5m sediment/peat sequence from Lake Pa Kho, northeast Thailand, which is supported by 20 AMS 14C ages. Hydroclimatic reconstructions for Pa Kho suggest a strengthened summer monsoon between BC 170-AD 370, AD 800-960, and after AD 1450; and a weakening of the summer monsoon between AD 370-800, and AD 1300-1450. Increased run-off and a higher nutrient supply after AD 1700 can be linked to agricultural intensification and land-use changes in the region. This study fills an important gap in data coverage with respect to summer monsoon variability over Southeast Asia during the past 2000 years and enables the mean position of the Intertropical Convergence Zone (ITCZ) to be inferred based on comparisons with other regional studies. Intervals of strengthened/weaker summer monsoon rainfall suggest that the mean position of the ITCZ was located as far north as 35°N between BC 170-AD 370 and AD 800-960, whereas it likely did not reach above 17°N during the drought intervals of AD 370-800 and AD 1300-1450. The spatial pattern of rainfall variation seems to have changed after AD 1450, when the inferred moisture history for Pa Kho indicates a more southerly location of the mean position of the summer ITCZ.
KW - Asian monsoon
KW - Geochemistry
KW - Last two millennia
KW - Paleoclimate
KW - Wetland/peatland
U2 - 10.1016/j.quascirev.2015.01.007
DO - 10.1016/j.quascirev.2015.01.007
M3 - Article
VL - 111
SP - 62
EP - 71
JO - Quaternary Science Reviews
T2 - Quaternary Science Reviews
JF - Quaternary Science Reviews
SN - 0277-3791
ER -