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Investigation of peat sediments from Daiyun Mountain in southeast China: late Holocene vegetation, climate and human impact


In this study, late Holocene vegetation, climate and human impacts were investigated using multiproxy data-pollen percentages, pollen accumulation rates (PAR), humification and loss-on-ignition (LOI)—measured from peat sediments from Daiyun Mountain, southeast China. A stratigraphic chronology was established on the basis of four radiocarbon dates. The 4,350 year sequence of vegetation history and climate change exhibits three distinctive stages: (1) 4,350–1,000 cal bp, during which the vegetation was dominated by evergreen forests mainly composed of broad-leaf trees, indicating a warm and wet climate; (2) 1,000–550 cal bp, during which the climate was thought to be cool and dry, based on a decrease in pollen percentages and the PARs of trees, shrubs and wetland herbs, and an increase in the pollen percentage and PAR of dry land herbs, as well as high overall LOI values; and (3) 550 cal bp to modern times, during which higher pollen percentages of dry land and wetland herbs, along with low pollen percentage and PAR of trees and shrubs, as well as low absorbance and LOI values, suggest relatively cooler but wetter climate conditions. In addition, major climatic events, such as the warm period from ad 670–960, the Medieval Warm Period (ad 1050–1520) and the Little Ice Age (ad 1580–1850), could be identified within the peat sediments in this study, with climatic conditions at these times being characteristically warm and wet, warm and dry, and cold and wet, respectively. Pollen signals indicate significant human impact since 1,000 cal bp, which may be linked to the development of the local porcelain industry and a rapid increase in the population in the study region.

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  1. Aaby B (1976) Cyclic climatic variations in climate over the past 5500 yr reflected in raised bogs. Nature 263:281–284

  2. Adhikari DP, Kumon F (2001) Climatic changes during the past 1,300 years as deduced from the sediments of Lake Nakatsuna, central Japan. Limnology 2:157–168

  3. Birks HJB (1998) D.G. Frey and E.S. Deevey review 1: numerical tools in palaeolimnology-progress, potentialities and problems. J Paleolimnol 20:307–332

  4. Birks HJB, Gordon AD (1985) Numerical methods in quaternary pollen analysis. Academic Press, London

  5. Blaauw M (2010) Methods and code for “classical” age modeling of radiocarbon sequences. Quat Geochronol 5:512–518

  6. Blackford JJ, Chambers FM (1993) Determining the degree of peat decomposition for peat-based paleaoclimatic studies. Int Peat 5:7–24

  7. Borgmark A (2005) Holocene climate variability and periodicities in south-central Sweden, as interpreted from peat humification analysis. Holocene 15:387–395

  8. Borgmark A, Schoning K (2006) A comparative study of peat proxies from two eastern central Swedish bogs and their relation to meteorological data. J Quat Sci 21:109–114

  9. Bradshaw RHW (1981) Quantitative reconstruction of local woodland vegetation using pollen analysis from a small basin in Norfolk, England. J Ecol 69:941–955

  10. Cai BQ (1998) The living environment and resource development in coastal of Fujian from the shell mound site. J Xiamen Univ 3:106–111 (In Chinese)

  11. Cao XY, Xu QH, Jing ZC, Tang JG, Li YC, Tian F (2010) Holocene climate change and human impacts implied from the pollen records in Anyang, central China. Quat Int 227:3–9

  12. Chen YS (1990) Forest fire in early Holocene forest changes at Lake Barrine, Australia. Acta Bot Sin 32:69–75 (In Chinese with English abstract)

  13. Chen JZ, Chen DL (2011) Dehua porcelain. Culture and Art Press, Beijing

  14. Chen WR, Lan DZ, Chen CH (1998a) Late Quaternary data and sea level changes in estuarine plain of the Jiulong River. Acta Oceanol Sin 20:65–72 (In Chinese with English abstract)

  15. Chen WR, Lan DZ, Chen CH, Yu YF (1998b) Sporo-pollen assemblages and climatic-environmental changes in Jiulongjiang Estuarine Plain during Late Quaternary. J Oceanogra Taiwan Strait 17:34–42 (In Chinese with English abstract)

  16. Chen W, Wang WM, Dai XR (2009) Holocene vegetation history with implications of human impact in the Lake Chaohu area, Anhui Province, East China. Veget Hist Archaeobot 18:137–146

  17. Chen JH, Chen FH, Feng S, Huang W, Liu JB, Zhou AF (2015) Hydroclimatic changes in China and surroundings during the medieval climate anomaly and little ice age: spatial patterns and possible mechanisms. Quat Sci Rev 107:98–111

  18. Chu GQ, Liu JQ, Sun Q, Lu HY, Gu ZY, Wang WY, Liu TS (2002) The ‘Mediaeval Warm Period’ drought recorded in Lake Huguangyan, tropical South China. Holocene 12:511–516

  19. Cichon M, Niedzielski P (2015) Dirt road: a geomorphological and geochemical record of Late-Holocene human activity in the catchment of Lake Radacz (Central Pomerania, Poland). Quat Int 370:145–158

  20. Cronin TM, Dwyer GS, Kamiya T, Schwede S, Willard DA (2003) Medieval Warm Period, Little Ice Age and 20th century temperature variability from Chesapeake Bay. Glob Planet Chang 36:17–29

  21. Daley TJ, Barber KE (2012) Multi-proxy Holocene palaeoclimate records from Walton Moss, northern England and Dosenmoor, northern Germany, assessed using three statistical approaches. Quat Int 268:111–127

  22. Dean WE (1974) Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods. J Sedim Petrol 44:242–248

  23. Driese SG, Ashley GM, Li ZH, Hoverc VC, Owen RB (2004) Possible Late Holocene equatorial palaeoclimate record based upon soils spanning the Medieval Warm Period and Little Ice Age, Loboi Plain, Kenya. Palaeogeogr Palaeoclimatol Palaeoecol 213:231–250

  24. Egli M, Mastrolonardo G, Seiler R, Raimondi S, Favilli F, Crimi V, Krebs R, Cherubini P, Certini G (2012) Charcoal and stable soil organic matter as indicators of fire frequency, climate and past vegetation in volcanic soils of Mt. Etna, Sicily. Catena 88:14–26

  25. Faust D, Zielhofer C, Escudero RB, Del Olmo FD (2004) High-resolution fluvial record of Late Holocene geomorphic change in northern Tunisia: climatic or human impact? Quat Sci Rev 23:1,757–1,775

  26. Ge QS, Zheng JY, Fang XQ, Man ZM, Zhang XQ, Zhang PY, Wang WQ (2002) Temperature changes of winter-half-year in eastern China during the past 2,000 years. Quat Sci 2:166–173 (In Chinese with English abstract)

  27. Grimm E (2011) Tilia and Tiliagraph software 1.7.16. Illinois State Museum, Springfield

  28. Huang KY, Zheng Z, Liao WB, Cao LL, Zheng YW, Zhang H, Zhu GQ, Zhang Z, Cheddadi R (2014) Reconstructing Late Holocene vegetation and fire histories in monsoonal region of southeastern China. Palaeogeogr Palaeoclimatol Palaeoecol 393:102–110

  29. Jacobson GL, Bradshaw RHW (1981) The selection of sites for palaeovegetational studies. Quat Res 16:80–96

  30. Jiang WY, Leroy SAG, Ogle N, Chu GQ, Wang L, Liu JQ (2008) Natural and anthropogenic forest fires recorded in the Holocene pollen record from a Jinchuan peat bog, northeastern China. Palaeogeogr Palaeoclimatol Palaeoecol 261:47–57

  31. Jin DS, Zheng F (1993) Palaeoclimate in the coastal area of central Fujian, 120,000 years bp. Geol Fujian 12:218–227 (In Chinese with English abstract)

  32. Lan DZ, Yu YF, Chen CH, Xie ZT (1986) Preliminary study on Late Pleistocene transgression and Holocene sea-level Fluctuation in Fuzhou Basin. Mar Geol Quat Geol 6:103–111 (In Chinese with English abstract)

  33. Li YY, Zhou LP, Cui HT (2008) Pollen indicators of human activity. Chin Sci Bull 53:1,281–1,293

  34. Li JY, Zhao Y, Xu QH, Zheng Z, Lv HY, Luo YL, Li YC, Li CH, Seppä H (2014) Human influence as a potential source of bias in pollen-based quantitative climate reconstructions. Quat Sci Rev 99:112–121

  35. Lin P (2002) A compressive report of Daiyun Mountain Natural Reserve in Fujian Province. Xiamen University Press, Fujian

  36. Liu KB, Qiu HL (1994) Late Holocene pollen records of vegetational changes in China: climate or human disturbance? Terr Atmos Ocean Sci 5:393–410

  37. Lv J, Wang YF, Li CS (2002) Fossil charcoal and ancient forest fire. J Palaeogeogr 4:71–76 (In Chinese with English abstract)

  38. Ma CM, Zhu C, Zheng ZG, Yin Q, Zhao ZP (2009) Climate changes in East China since the Late-glacial inferred from high-resolution mountain peat humification records. Sci China Ser D 52:118–131

  39. Maher LJ (1981) Statistics for microfossil concentration measurements employing samples spiked with marker grains. Rev Palaeobot Palynol 32:153–191

  40. Mann ME, Jones PD (2003) Global surface temperatures over the past two millennia. Geophys Res Lett 30:18–20

  41. Marquer L, Pomel S, Abichou A, Schulz E, Kaniewski D, Campo EV (2008) Late Holocene resolution palaeoclimatic reconstruction inferred from Sebkha Mhabeul, southeast Tunisia. Quat Res 70:240–250

  42. Matul AG, Khusid TA, Mukhina VV, Chekhovskaya MP, Safarova SA (2007) Recent and late Holocene environments on the southeastern shelf of the Laptev Sea as inferred from microfossil data. Oceanology 47:80–90

  43. Minckley T, Whitlock C, Bartlein P (2007) Vegetation, fire, and climate history of the northwestern Great Basin during the last 14,000 years. Quat Sci Rev 26:2167–2184

  44. Nakagawa T, Brugiapaglia E, Digerfeldt G, Reille M, De Beaulieu JL, Yasuda Y (1998) Dense-media separation as a more efficient pollen extraction method for use with organic sediment samples: comparison with the conventional method. Boreas 25:15–24

  45. Nielsen AB, Sugita S (2005) Estimating relevant source area of pollen for small Danish lakes around ad 1800. Holocene 15:1006–1020

  46. Patterson WA, Edwards KJ, Maquire DJ (1987) Microscopic charcoal as a fossil indicator fire. Quat Sci Rev 6:3–23

  47. Pla S, Catalan J (2005) Chrysophyte cysts from lake sediments reveal the sub millennial winter/spring climate variability in the northwestern Mediterranean region throughout the Holocene. Clim Dyn 24:263–278

  48. Prentice IC (1985) Pollen representation, source area, and basin size: toward a unified theory of pollen analysis. Quat Res 23:76–86

  49. Qiu HL (2006) A 4000 year pollen record of vegetation change from the subtropical mountains of Fujian Province, China. J Subtrop Resour Environ 1:11–23

  50. Qu XL, Chen ZY (2010) The reasons of shell mound sites disappeared by comparison of the Shandong Peninsula and the coastal Fujian. Fujian Fair 2:6–11

  51. Quamar MF, Chauhan MS (2014) Signals of Medieval Warm Period and Little Ice Age from southwestern Madhya Pradesh (India): a pollen-inferred Late-Holocene vegetation and climate change. Quat Int 325:74–82

  52. Reimer PJ, Baillie MGL, Bard E et al (2009) INTCAL 09 and MARINE09 radiocarbon age calibration curves, 0-50,000 years cal bp. Radiocarbon 51:1111–1150

  53. Sadori L, Giardini M (2007) Charcoal analysis, a method to study vegetation and climate of the Holocene: the case of Lago di Pergusa (Sicily, Italy). Geobios 40:173–180

  54. Sadori L, Giardini M, Gliozzi E, Mazzini I, Sulpizio R, Van Welden A, Zanchetta G (2015) Vegetation, climate and environmental history of the last 4500 years at lake Shkodra (Albania/Montenegro). Holocene 25:435–444

  55. Shao XH, Wang YJ, Cheng H, Kong XG, Wu JY, Lawrence ER (2006) Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China. Chin Sci Bull 51:80–86

  56. Stuiver M, Reimer PJ (1993) Extended 14C data base and revised Calib 3.0 14C age calibration program. Radiocarbon 35:215–230

  57. Stuiver M, Reimer PJ, Bard E et al (1998) Intcal 98 Radiocarbon age calibration 24000–0 cal bp. Radiocarbon 40:1,041–1,083

  58. Tan LC, Cai YJ, Cheng H, An ZS, Edwards RL (2009) Summer monsoon precipitation variations in central China over the past 750 years derived from a high resolution absolute-dated stalagmite. Palaeogeogr Palaeoclimatol Palaeoecol 280:432–439

  59. Tarasov PE, Jin GY, Wagner M (2006) Mid-Holocene environmental and human dynamics in northeastern China reconstructed from pollen and archaeological data. Palaeogeogr Palaeoclimatol Palaeoecol 241:284–300

  60. Ter Braak CJF, Smilauer P (2003) Canoco for Windows v. 4.52. Biometris, Wageningen

  61. Tian ZH, Han YM, Cao JJ, Huang CC, An ZS (2015) Holocene wildfire history and human activity from high-resolution charcoal and elemental black carbon records in the Guanzhong Basin of the Loess Plateau, China. Quat Sci Rev 109:76–87

  62. Turner TE, Swindles GT, Roucoux KH (2014) Late Holocene ecohydrological and carbon dynamics of a UK raised bog: impact of human activity and climate change. Quat Sci Rev 84:65–85

  63. Van der Linden M, Barke J, Vickery E, Charman DJ, Van Geel B (2008) Late Holocene human impact and climate change recorded in a North Swedish peat deposit. Palaeogeogr Palaeoclimatol Palaeoecol 258:1–27

  64. Viau AE, Ladd M, Gajewski K (2012) The climate of North America during the past 2,000 years reconstructed from pollen data. Glob Planet Chang 84–85:75–83

  65. Wang SW (2010) Medieval warm period and little ice age. Adv Clim Chang Res 6(5):388–390 (In Chinese)

  66. Wang YB, Herzschuh U (2011) Reassessment of Holocene vegetation change on the upper Tibetan Plateau using the pollen-based REVEALS model. Rev Palaeobot Palynol 168:31–40

  67. Wang FX, Qian NF, Zhang YL (1995a) Pollen flora of China. Science Press, Beijing

  68. Wang KF, Lu JJ, Zheng YL (1995b) Late Quaternary pollen-diatom assemblages along Fujian seashore and their palaeoenvironmental implication. Acta Micropalaeontol Sin 12:388–397 (In Chinese with English abstract)

  69. Wang YJ, Cheng H, Edwards RL, He YQ, Kong XG, An ZS, Wu JY, Kelly MJ, Dykoski CA, Li XD (2005) The Holocene Asian monsoon: links to solar changes and North Atlantic climate. Science 308:854–857

  70. Wang SY, Lu HY, Liu JQ, Negendank Jörg FW (2007) The early Holocene optimum inferred from a high-resolution pollen record of Huguangyan Maar Lake in southern China. Chin Sci Bull 52:2,829–2,836

  71. Wang YJ, Cheng H, Edwards RL et al (2008) Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451:1,090–1,093

  72. Wu XZ (1993) Holocene sporopollen assemblage in Mawei, Fuzhou City and their geological significance. Geol Fujian 4:292–299 (In Chinese with English abstract)

  73. Wu XD, Zhang ZH, Xu XM, Shen J (2012) Asian summer monsoonal variations during the Holocene revealed by Huguangyan Maar lake sediment record. Palaeogeogr Palaeoclimatol Palaeoecol 323–325:13–21

  74. Xi YZ, Ning JZ (1994) Pollen morphology of arid and semi-arid regions of China. Yushan Biol 11:119–191 (In Chinese with English abstract)

  75. Xu QH, Zhang SR (2013) Advance in pollen source area. Adv Earth Sci 28:968–975 (In Chinese with English abstract)

  76. Xu JX, Zheng Z, Huang KY, Yue YY, Li J, Chase BM, Ledru MP, Carré M, Cheddadi R (2013) Impacts of human activities on ecosystems during the past 1,300 years in Pingnan area of Fujian Province, China. Quat Int 286:29–35

  77. Yancheva G, Nowaczyk NR, Mingram J et al (2007) Influence of the intertropical convergence zone on the East Asian monsoon. Nature 445:74–77

  78. Yang B, Bräuning A, Shi YF (2003) Late Holocene temperature fluctuations on the Tibetan Plateau. Quat Sci Rev 22:2,335–2,344

  79. Yang B, Bräuning A, Yao TD, Davis ME (2007) Correlation between the oxygen isotope record from Dasuopu ice core and the Asian Southwest Monsoon during the last millennium. Quat Sci Rev 26:1,810–1,817

  80. Yue YF, Zheng Z, Huang KY, Chevalier M, Chase BM, Carré M, Ledru MP, Cheddadi R (2012) A continuous record of vegetation and climate change over the past 50,000 years in the Fujian Province of eastern subtropical China. Palaeogeogr Palaeoclimatol Palaeoecol 365–366:115–123

  81. Yue YF, Zheng Z, Rolett BV, Ma T, Chen C, Huang KY, Lin GW, Zhu GQ, Cheddadi R (2014) Holocene vegetation, environment and anthropogenic influence in the Fuzhou Basin, southeast China. J Asian Earth Sci 99:85–94

  82. Zeng Y, Chen JG, Zhu ZJ, Li J, Wang JF, Wan GJ (2012) The wet Little Ice Age recorded by sediments in Huguangyan Lake, tropical South China. Quat Int 263:55–62

  83. Zhang JH, Kong ZC, Du NQ (1998) The respondence of Loss-on-ignition range to past climate and environment in Beijing. Acta Ecol Sin 18:343–347 (In Chinese with English abstract)

  84. Zhang PZ, Cheng H, Edwards RL, Chen FH, Wang YJ, Yang XL, Liu J, Tan M, Wang XF, Liu JH (2008) A test of climate, sun, and culture relationships from an 1,810-year Chinese cave record. Science 322:940–942

  85. Zhang Y, Liu XT, Lin QX, Gao CY, Wang J, Wang GP (2014) Vegetation and climate change over the past 800 years in the monsoon margin of northeastern China reconstructed from n-alkanes from the Great Hinggan Mountain ombrotrophic peat bog. Org Geochem 76:128–135

  86. Zhao ZY, Yuan DX, Shi SQ, Luo LD (2012) MIS3b vegetation and climate changes based on pollen and charcoal on Qianxi Plateau. Acta Ecol Sin 32:4,811–4,818 (In Chinese with English abstract)

  87. Zheng Z (1991) Pollen flora and palaeoclimate of the Chaoshan Plain during the last 50,000 years. Acta Micropalaeontol Sin 8:461–480 (In Chinese with English abstract)

  88. Zheng RZ, Xu XW, Zhu JF, Ji FJ, Huang ZL, Li JP (2002) Division of Late Quaternary strata and analysis of palaeoenvironment in Fuzhou basin. Seismol Geol 24:503–513 (In Chinese with English abstract)

  89. Zhi CY, Wang KF, Lan DZ, Chen CH, Zheng YL (2003) Study on the relationship between diatom assemblage and palaeoenvironment of the Late Quaternary in the Taiwan Channel and Xinmen Island. Acta Micropalaeontol Sin 20:244–252 (In Chinese with English abstract)

  90. Zhou WJ, Donahue D, Jull AJ (1997) Radiocarbon AMS dating of pollen concentrated from eolian sediments. Radiocarbon 39:19–26

  91. Zhou WJ, Yu XF, Jull AJT, Burr G, Xiao JY, Lu XF, Xian F (2004) High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the past 18000 years. Quat Res 62:39–48

  92. Zhou WJ, Xie SC, Meyers PA, Zheng YH (2005) Reconstruction of Late glacial and Holocene climate evolution in southern China from geolipids and pollen in the Dingnan peat sequence. Org Geochem 36:1,272–1,284

  93. Zhu KZ (1973) Preliminary studies of climate change in China nearly five thousand years. Chin Sci Bull 2:168–189 (In Chinese)

  94. Zuo XX, Jin HL (2009) An overview of studies on Medieval Warm Period. J Desert Res 1:136–142 (In Chinese with English abstract)

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We are grateful to the staff of the Daiyun Mountain National Nature Reserve for access permission and Wei Shi, Feixue Feng and Dang Li for assistance during the field work. We thank the editor and two anonymous reviewers for their helpful comments and suggestions that improved the manuscript. This research was jointly funded by the National Natural Science Foundation of China (NSFC, No. 41371202), the Strategic Priority Research Program of the Chinese Academy of Sciences (XDA05120704), 973 Program under Grant (No.2015CB953800) and the open-ended fund (SKLLQG1313) from the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment of the China Academy of Sciences.

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Correspondence to Chunmei Ma.

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Communicated by Y. Zhao.

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Zhao, L., Ma, C., Tang, L. et al. Investigation of peat sediments from Daiyun Mountain in southeast China: late Holocene vegetation, climate and human impact. Veget Hist Archaeobot 25, 359–373 (2016). https://doi.org/10.1007/s00334-016-0554-2

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  • Late holocene
  • Vegetation
  • Climate change
  • Human impact
  • Peat
  • Daiyun Mountain