Abstract
Palaeoecological analyses including pollen and charcoal analyses on a sediment core (NP3) collected from Nong Pling freshwater spring area in Thong Pha Phum, western Thailand are used to reconstruct past environmental change. The results demonstrate that there were changes in plant composition over the past 700 years resulting from interactions between hydrological conditions in relation to rainfall variability, and anthropogenic activity. Open vegetation such as grasses and lowland forest were established in Nong Pling freshwater spring forest from at least around ad 1300 suggesting drier conditions than present until around ad 1460. After that, decreased lowland forest and increased freshwater spring taxa together with the low charcoal contents indicate wetter conditions than during the former period, which allowed freshwater spring taxa to establish until around ad 1800. There were some fluctuations between freshwater spring taxa and lowland forest with open vegetation, probably due to rainfall fluctuations particularly after ad 1800 until the present. Moreover, recent increases in total charcoal accumulation, especially in large particles and the appearance of domesticated grass pollen may be related to recent human interaction within the ecosystems in Thong Pha Phum.
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References
Anderson DM, Overpeck JT, Gupta AK (2002) Increase in the Asian Southwest Monsoon during the past four centuries. Science 297(5581):596–599
Anderson DM, Baulcomb CK, Duvivier AK, Gupta AK (2010) Indian summer monsoon during the last two millennia. J Quat Sci 25:911–917
Baker C, Phongpaichit P (2014) A history of Thailand. Cambridge University Press, Cambridge
Beamish FWH (2007) Thong Pha Phum; synthesis of the aquatic projects with a view to the future. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 7–12
Benninghoff WS (1962) Calculation of pollen and spores density in sediments by addition of exotic pollen in known quantities. Pollen Spores 4:332–333
Blaauw M, Heegaard E (2012) Estimation of age-depth relationships. In: Birks HJB, Juggins S, Lotter A, Smol JP (eds) Tracking environmental change using lake sediments, developments in paleoenvironmental research vol 5: data handling and statistical techniques. Springer, Dordrecht, pp 379–413
Boonkerd T (2007) Overview of plant research in western Thong Pha Phum Project. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 99–109
Boonkerd T, Pollawatn R (2006) Pteridophyte Flora of Thong Pha Phum National Park, Kanchanaburi Province, Thailand. Nat Hist J Chulalongkorn Univ 6:17–30
Bronk-Ramsey C (2009) OxCal Program v4.10. Oxford Radiocarbon Accelerator Unit, Oxford
Buckley BM, Palakit K, Duangsathaporn K, Sanguantham P, Prasomsin P (2007) Decadal scale droughts over northwestern Thailand over the past 448 years: links to the tropical Pacific and Indian Ocean sectors. Clim Dyn 29:63–71
Buckley BM, Anchukaitis KJ, Penny D et al (2010) Climate as a contributing factor in the demise of Angkor. Cambodia Proc Nat Acad Sci 107(15):6748–6752
Buckley BM, Fletcher R, Wang S-YS, Zottoli B, Pottier C (2014) Monsoon extremes and society over the past millennium on mainland Southeast Asia. Quat Sci Rev 95:1–19
Bunopas S (1982) Paleogeographic history of western Thailand and adjacent parts of South-east Asia: a plate tectonics interpretation. Geological Survey Paper 5. Geological Survey Division, Department of Mineral Resources, Bangkok
Carcaillet C, Bouvier M, Fréchette B, Larouche AC, Richard PJ (2001) Comparison of pollen-slide and sieving methods in lacustrine charcoal analyses for local and regional fire history. Holocene 11:467–476
Chaturvedi M, Datta K, Nair PK (1998) Pollen morphology of Oryza (Poaceae). Grana 37:79–86
Chawchai S, Chabangborn A, Fritz S et al (2015) Hydroclimatic shifts in northeast Thailand during the last two millennia—the record of Lake Pa Kho. Quat Sci Rev 111:62–71
Chen F-H, Chen B, Zhao Y, Zhu Y, Madson DB (2006) Holocene environmental change inferred from high-resolution pollen records from inland lake deposits, arid China. Holocene 16:675–684
Clark JS (1988) Particle motion and the theory of stratigraphic charcoal analysis: source area, transport, deposition, and sampling. Quat Res 30:67–80
Cohen MCL, Behling H, Lara RJ (2005) Amazonian mangrove dynamics during the last millennium: the relative sea-level and the Little Ice Age. Rev Palaeobot Palynol 136:93–108
Conedera M, Tinner W, Neff C, Meurer M, Dickens AF, Krebs P (2009) Reconstructing past fire regimes: methods, applications, and relevance to fire management and conservation. Quat Sci Rev 28:555–576
Cook ER, Anchukaitis KJ, Buckley BM, D’Arrigo RD, Wright WE, Jacoby GC (2010) Asian monsoon failure and megadrought during the last millennium. Science 328(5977):486–489
Crowley GM, Grindrod J, Kershaw AP (1994) Modern pollen deposition in the tropical lowlands of northeast Queensland, Australia. Rev Palaeobot Palynol 83:299–327
Daniau AL, Harrison SP, Bartlein PJ (2010) Fire regimes during the last glacial. Quat Sci Rev 29:2918–2930
Darumas P, Khunwasi C, Seelanan T (2007) Diversity of vascular plants in spring water swamp areas of Thong Pha Phum District, Kanchanaburi Province, Thailand. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 128–145
Erdtman G (1969) Handbook of palynology. Hafner, New York
Faegri K, Iversen J (1989) Textbook of pollen analysis. Wiley, Chichester
Gorman C (1971) The Hoabinhian and after: subsistence patterns in Southeast Asia during the late Pleistocene and early recent periods. World Archaeol 2:300–320
Grimm EC (1991) Tilia and tiliagraph. Illinois State Museum, Springfield
Hammond AP, Goh KM, Tonkin PJ, Manning MR (1991) Chemical pretreatments for improving the radiocarbon dates of peats and organic silts in a gley podzol environment: Grahams Terrace, North Westland. N Z J Geol Geophys 34:191–194
Jardine PE, Lomax BH (2017) Is pollen size a robust proxy for moisture availability? Rev Palaeobot Palynol 246:161–166
Jardine PE, Gosling WD, Lomax BH, Julier ACM, Fraser WT (2019) Chemotaxonomy of domesticated grasses: a pathway to understanding the origins of agriculture. J Micropalaeont 38:83–95
Johansen B, von Bothmer R (1994) Pollen size in Hordeum L.: correlation between size, ploidy level, and breeding system. Sex Plant Reprod 7:259–263
Joly C, Barillé L, Barreau M, Mancheron A, Visset L (2007) Grain and annulus diameter as criteria for distinguishing pollen grains of cereals from wild grasses. Rev Palaeobot Palynol 146:221–233
Kealhofer L, Penny D (1998) A combined pollen and phytolith record for fourteen thousand years of vegetation change in northeastern Thailand. Rev Palaeobot Palynol 103:83–93
Kengkarj P, Chalermglin P, Srithongkuland J, Phiriyaphattharakit A (2007) Sustainable utilization of vascular plants and rural technology transfer in west Thong Pha Phum. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 249–254
Kershaw AP (1997) A modification of the Tröels-Smith system of sediment description and portrayal. Quat Australasia 15:63–68
Khonsue W (2007) Species diversity of amphibian in Thong Pha Phum District, Kanchanaburi Province. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 312–320
Land Development Department (2011) Landuse data in Thailand year 2011. Land Development Department, Ministry of Agriculture and Co-operatives, Bangkok
Lieberman V, Buckley B (2012) The impact of climate on Southeast Asia, circa 950–1820: new findings. Mod Asian Stud 46:1049–1096
Lynch JA, Clark JS, Stocks BJ (2004) Charcoal production, dispersal, and deposition from the Fort Providence experimental fire: interpreting fire regimes from charcoal records in boreal forests. Can J Forest Res 34:1642–1656
Maloney BK (1991) Rice agricultural origins: recent advances. GeoJournal 23:121–124
Mauquoy D, van Geel B, Blaauw M, Speranza A, van der Plicht J (2004) Changes in solar activity and Holocene climate shifts derived from 14C wiggle-match dated peat deposits. Holocene 14:45–52
Meteorological Department (2003) Climatological data from Thong Pha Phum Climatic Station, Kanchanaburi Province, 1973–2003. DataProcessing Subdivision, Climatology Division, Meteorological Department, Bangkok
Moore PD, Webb JA, Collison ME (1991) Pollen analysis. Blackwell Scientific Publications, Oxford
Nutalaya P, Campbell KV, Macdonald AS (1979) Review of the geology of Thai tin fields. Geol Soc Malaysia Bull 11:137–159
Pearson FJ, Hanshaw BB (1970) Sources of dissolved carbonate species in groundwater and their effects on carbon-14 dating. Isotope hydrology. IAEA, Vienna, pp 271–285
Prayong N, Srikosamatara S (2007) Status of small carnivore in PTT forest reserve, Thong Pha Phum District, Kanchanaburi Province: a guideline for local community involvement in wildlife management. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 379–384
Pumijumnong N, Eckstein D (2011) Reconstruction of pre-monsoon weather conditions in northwestern Thailand from the tree-ring widths of Pinus merkusii and Pinus kesiya. Trees 25:125–132
Reimer PJ, Bard E, Bayliss A et al (2013) IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55:1869–1887
Ridd MF, Barber AJ, Crow MJ (eds) (2011) The geology of Thailand. Geological Society of London, London
Rucina SM, Muiruri VM, Kinyanjui RN, McGuiness K, Marchant R (2009) Late Quaternary vegetation and fire dynamics on Mount Kenya. Palaeogeogr Palaeoclimatol Palaeoecol 283:1–14
Rull V, Abbott MB, Polissar PJ, Wolfe AP, Bezada M, Bradley RS (2005) 15,000-yr pollen record of vegetation change in the high altitude tropical Andes at Laguna Verde Alta, Venezuela. Quat Res 64:308–317
Sarapirome S, Surinkum A, Saksutthipong P (2002) Application of DEM data to geological interpretation: Thong Pha Phum area, Thailand. 23rd Asian Conference on Remote Sensing, November. Birenda International Convention Centre, Kathmandu, pp 25–29
Shoocongdej R (1996) Rethinking the development of sedentary villages in western Thailand. Bull IndoPacific Prehist Assoc 14:203–215
Srapratet S (2002) Diversity of Vascular Plants at Springs in Moo Ban Tha Ma Dua. Thong Pha Phum District. Kanchanaburi Province. Master Thesis. Chulalongkorn University, Bangkok
Srapratet S, Seelanan T, Na Songkhla B (2007) Diversity of vascular plants at springs in Moo Ban Tha Ma Dua, Thong Pha Phum District, Kanchanaburi Province. In: Baimai V, Tanthalakha R (eds) BRT research reports 2007: western Thong Pha Phum. Jirawat Express, Bangkok, pp 168–178
Tierney JE, Oppo DW, Rosenthal Y, Russell JM, Linsley BK (2010) Coordinated hydrological regimes in the Indo-Pacific region during the past two millennia. Paleoceanogr 25:PA1102
Tinner W, Hu FS (2003) Size parameters, size-class distribution and area-number relationship of microscopic charcoal: relevance for fire reconstruction. Holocene 13:499–505
Troels-Smith J (1955) Characterisation of unconsolidated sediments. Danmarks Geologiske Undersøgelse 3:7–73
Van der Kaars S, Penny D, Tibby J, Fluin J, Dam RA, Suparan P (2001) Late Quaternary palaeoecology, palynology and palaeolimnology of a tropical lowland swamp: Rawa Danau, West-Java, Indonesia. Palaeogeogr Palaeoclimatol Palaeoecol 171:185–212
Vandergoes MJ, Prior CA (2003) AMS dating of pollen concentrates—a methodological study of late Quaternary sediments from south Westland, New Zealand. Radiocarbon 45:479–491
Whitlock C, Larsen C (2001) Charcoal as a fire proxy. In: Smol JP, Birks HJB, Last WM (eds) Tracking environmental change using Lake Sediments vol 3: terrestrial, algal, and siliceous indicators. Springer, Dordrecht, pp 75–97
Willis KJ, Birks HJB (2006) What is natural? The need for a long-term perspective in biodiversity conservation. Science 314:1261–1265
Wohlfarth B, Higham C, Yamoah KA, Chabangborn A, Chawchai S, Smittenberg RH (2016) Human adaptation to mid-to late-Holocene climate change in Northeast Thailand. Holocene 26:1875–1886
Wongwanich T, Tansathien W, Leevongcharoen S, Paengkaew W, Thiamwong P, Chaeroenmit J, Saengsrichan W (2002) The Lower Paleozoic rocks of Thailand. Proceedings of the Symposium on Geology of Thailand. Department of Mineral Resources Bangkok, Bangkok, pp 16–21
Yamoah KA, Chabangborn A, Chawchai S, Schenk F, Wohlfarth B, Smittenberg RH (2016) A 2000-year leaf wax-based hydrogen isotope record from Southeast Asia suggests low frequency ENSO-like teleconnections on a centennial timescale. Quat Sci Rev 148:44–53
Yamoah KA, Higham CF, Wohlfarth B, Chabangborn A, Chawchai S, Schenk F, Smittenberg RH (2017) Societal response to monsoonal fluctuations in NE Thailand during the demise of Angkor Civilisation. Holocene 27:1455–1464
Acknowledgements
Appreciation is expressed to Yotesawate Sirichamorn, Thanikarn Udomchalothorn, undergraduate students from the Faculty of Environment and Resource Studies, staff from the Forest Industry Organization, Thong Pha Phum, Mr Sampan Tongnunui and the local people for their support and assistance throughout the fieldwork. I also would like to thank Sakonvan Chawchai for valuable comments and suggestions for improving this manuscript and all the staff at the Faculty of Environment and Resource Studies, for support in the laboratory and faculty in general and also those at the Department of Plant Science, Faculty of Science. This research project is supported by Mahidol University.
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Punwong, P., Englong, A., Traiperm, P. et al. Vegetation history and human impacts from Thong Pha Phum, western Thailand during the past 700 years. Veget Hist Archaeobot 30, 383–394 (2021). https://doi.org/10.1007/s00334-020-00786-y
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DOI: https://doi.org/10.1007/s00334-020-00786-y