Skip to main content
Log in

Different climatic controls of soil δ 13Corg in three mid-latitude regions of the Northern Hemisphere since the Last Glacial period

  • Articles
  • Published:
Chinese Science Bulletin

Abstract

Paleoecological records of soil δ 13Corg from three regions in the middle latitudes of the Northern Hemisphere, including the Chinese Loess Plateau (CLP), the Great Plains and adjacent areas of North America and northwestern Europe, showed different variations since the Last Glacial period. An attempt was made to evaluate the causes for the difference in δ 13Corg on the basis of the modern climatic data collected in these regions and of the modern C3 and C4 plant distributions. The analysis indicates that temperature, especially the growing season temperature, has a dominant control on the growth of C4 plants. When the mean annual or growing season temperatures are below the “threshold value”, the growth of C4 plants is limited. When the temperature is above the “threshold value”, C4 plants can grow under a wide range of precipitation. However, when the precipitation is high enough to favor the growth of trees, the proportions of C4 plants in local biomass will decline. The implicit control factor recovered by sedimentary records is consistent with the control factor on modern C3/C4 distribution. Pure C3 plants have been dominating the local biomass since the Last Glacial period in European loess region, mainly owing to the low local temperature. The increases in C4 plants from the late Pleistocene to the Holocene in the Chinese Loess Plateau, the Great Plains and adjacent areas, mainly reflect the influence of increasing temperature.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Cerling T E, Harris J M, MacFadden B J, et al. Global vegetation change through the Miocene/Pliocene boundary. Nature, 1997, 389: 153–158

    Article  Google Scholar 

  2. Cerling T E, Wang Y, Quade J. Expansion of C4 ecosystems as an indicator of global ecological change in the late Miocene. Nature, 1993, 361: 344–345

    Article  Google Scholar 

  3. Ehleringer J R, Sage R F, Flanagan L B, et al. Climate Change and the Evolution of C4 Photosynthesis. Trends Ecol Evol, 1991, 6: 95–99

    Article  Google Scholar 

  4. Pagani M, Freeman K H, Arthur M A. Late Miocene atmospheric CO2 concentration and the expansion of C4 grasses. Science, 1999, 285: 876–879

    Article  Google Scholar 

  5. Huang Y, Street-Perrott F A, Metcalfe S E, et al. Climate change as the dominant control on glacial-interglacial variation in C3 and C4 plant abundance. Science, 2001, 293: 1647–1651

    Article  Google Scholar 

  6. Street-Perrott F A, Huang Y S, Perrott R A, et al. Impact of lower atmospheric carbon dioxide on tropical mountain ecosystems. Science, 1997, 278: 1422–1426

    Article  Google Scholar 

  7. Mora G, Pratt L M. Carbon isotopic evidence from paleosols for mixed C3/C4 vegetation in the Bogota Basin, Colombia. Quat Sci Rev, 2002, 21: 985–995

    Article  Google Scholar 

  8. Nordt L C, Boutton T W, Hallmark C T, et al. Late Quaternary vegetation and climate changes in Central Texas based on the isotopic composition of organic carbon. Quat Res, 1994, 41: 109–120

    Article  Google Scholar 

  9. Yamada K, Ishiwatari R. Carbon isotopic composition of long-chain n-alkanes in the Japan Sea sediments: implication for paleoenvironmental changes over the past 85 kyr. Org Geochem, 1999, 30: 367–377

    Article  Google Scholar 

  10. Liu W G, Ning Y F, An Z S. et al. Carbon isotopic composition of modern soil and paleosol as a response to vegetation change on the Chinese Loess Plateau. Sci China Ser D-Earth Sci, 2005, 48(1): 93–99

    Article  Google Scholar 

  11. Krishnamurthy R V, Bhattacharya S K. Paleovegetational history in the Kashmir Basin, India, derived from 13C/12C ratio in paleosols. Earth Planet Sci Lett, 1989, 95: 291–296

    Article  Google Scholar 

  12. Brincat D, Yamada K, Ishiwatayi R, et al. Molecular-isotopic stratigraphy of long-chain n-alkanes in Lake Baikal Holocene and glacial age sediments. Org Geochem, 2000, 31: 287–294

    Article  Google Scholar 

  13. Hatté C, Fontugne M, Rousseau D D, et al. δ13C variations of loess organic matter as a record of the vegetation response to climatic changes during the Weichselian. Geology, 1998, 26: 583–586

    Article  Google Scholar 

  14. Gu Z Y, Liu Q, Xu B, et al. Climate as the dominant control on C3 and C4 plant abundance in the Loess Plateau: Organic carbon isotope evidence from the last glacial-interglacial loess-soil sequences. Chin Sci Bull, 2003, 48(12): 1271–1276

    Article  Google Scholar 

  15. Liu W G, Huang Y S, An Z S, et al. Summer monsoon intensity controls C4/C3 plant abundance during the last 35 ka in the Chinese Loess Plateau: Carbon isotope evidence from bulk organic matter and individual leaf waxes. Palaeogeogr Palaeoclimatol Palaeoecol, 2005, 220: 243–254

    Article  Google Scholar 

  16. Vidic N J, Montañez I P. Climatically driven glacial-interglacial variations in C3 and C4 plant proportions on the Chinese Loess Plateau. Geology, 2004, 32: 337–340

    Article  Google Scholar 

  17. Zhang Z H, Zhao M X, Lu H Y, et al. Lower temperature as the main cause of C4 plant declines during the glacial periods on the Chinese Loess Plateau. Earth Planet Sci Lett, 2003, 214: 467–481

    Article  Google Scholar 

  18. Chen F H, Rao Z G, Zhang J W, et al. Variations of organic carbon isotopic composition and its environmental significance during the last glacial period on western Chinese Loess Plateau. Chin Sci Bull, 2006, 51(13): 1593–1602

    Article  Google Scholar 

  19. Nordt L C, Boutton T W, Jacob J S, et al. C4 plant productivity and climatie—CO2 variations in South-Central Texas during the late Quaternary. Quat Res, 2002, 58: 182–188

    Article  Google Scholar 

  20. Johnson W C, Willey K L. Isotopic and rock magnetic expression of environmental change at the Pleistocene — Holocene transition in the central Great Plains. Quat Int, 2000, 67: 89–106

    Article  Google Scholar 

  21. Kelly E F, Amundson R G, Marino B D, et al. Stable isotope ratios of carbon in phytoliths as a quantitative method of monitoring vegetation and climate change. Quat Res, 1991, 35: 222–233

    Article  Google Scholar 

  22. Panno S V, Curry B B, Wang H, et al. Climate change in southern Illinois, USA, based on the age and δ13C of organic matter in cave sediments. Quat Res, 2004, 301–313

  23. Fredlund G G, Tieszen L L. Phytolith and carbon isotope evidence for late Quaternary vegetation and climate change in the Southern Black Hills, South Dakota. Quat Res, 1997, 47: 206–217

    Article  Google Scholar 

  24. Hatté C, Antoine P, Fontugne M, et al. New chronology and organic matter δ13C paleoclimatic significance of Nußloch loess sequence (Rhine Valley, Germany). Quat Int, 1999, 62, 85–91

    Article  Google Scholar 

  25. Hatté C, Antoine P, Fontugne M, et al. δ13C of loess organic matter as a potential proxy for paleoprecipitation. Quat Res, 2001, 55: 33–38

    Article  Google Scholar 

  26. Stewart G R, Turnbull M H, Schmidt S, et al. 13C natural abundance in plant communities along a rainfall gradient: A biological integrator of water availability. Aust J Plant Physiol, 1995, 22: 51–55

    Article  Google Scholar 

  27. Wang G A, Han J M, Liu T S. The carbon isotope composition of C3 herbaceous plants in loess area of northern China. Sci China Ser D-Earth Sci, 2003, 46(10): 1069–1076

    Article  Google Scholar 

  28. Sage R F, Wedin D A, Li M R. The biogeography of C4 photosynthesis: patterns and controlling factors. In: Sage R F, Monson R K, C4 Plant Biology, Academic Press, San Diego, California, 1999, 313–373

    Google Scholar 

  29. Tieszen L L, Reed B C, Bliss L B, et al. NDVI, C3 and C4 production and distributions in Great Plains grassland land cover classes. Ecol Appl, 1997, 7(1): 59–78

    Article  Google Scholar 

  30. Lü H Y, Wang Y J, Wang G A, et al. Analysis of carbon isotope in phytoliths from C3 and C4 plants and modern soils. Chin Sci Bull, 2000, 45(19): 1804–1808

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Rao ZhiGuo.

Additional information

Supported by the National Natural Science Foundation of China (Grant No. 40331009), the Knowledge Innovation Programs of Chinese Academy of Sciences (Grant No. KZCX3-SW-152) and the National Basic Research Program of China (Grant Nos. 2003CCA00100, 2004 CB720 204)

About this article

Cite this article

Rao, Z., Zhu, Z. & Zhang, J. Different climatic controls of soil δ 13Corg in three mid-latitude regions of the Northern Hemisphere since the Last Glacial period. CHINESE SCI BULL 52, 259–266 (2007). https://doi.org/10.1007/s11434-007-0006-6

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11434-007-0006-6

Keywords

Navigation