Articles | Volume 4, issue 1
Clim. Past, 4, 1–9, 2008
https://doi.org/10.5194/cp-4-1-2008
Clim. Past, 4, 1–9, 2008
https://doi.org/10.5194/cp-4-1-2008

  02 Jan 2008

02 Jan 2008

Changes in C3/C4 vegetation in the continental interior of the Central Himalayas associated with monsoonal paleoclimatic changes during the last 600 kyr

M. Mampuku1, T. Yamanaka1,*, M. Uchida2,**, R. Fujii1,***, T. Maki1,****, and H. Sakai1,*** M. Mampuku et al.
  • 1Dept. Evol. Earth Environ., SCS, Kyushu University, Ropponmatsu, Fukuoka 810-8560, Japan
  • 2IORGC, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 237-0061, Japan
  • *now at: Div. Earth Sci., Grad. School Natural Sci. Tech., Okayama University, Okayama 700-8530, Japan
  • **now at: Environmental Chemistry Division, National Institute for Environmental Studies, Tsukuba 305-8560, Japan
  • ***now at: Div. Earth Planet. Sci., Grad. School Sci., Kyoto Univ., Kyoto, 606-8502, Japan
  • ****now at: CDEX, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama 236-0001, Japan

Abstract. A continuous lacustrine sediment core obtained from the Kathmandu Valley in the Central Himalayas revealed that cyclical changes in C3/C4 vegetation corresponded to global glacial-interglacial cycles from marine isotope stages (MIS) 15 to MIS 4. The C3/C4 vegetation shifts were reconstructed from significant changes in the δ13C values of bulk organic carbon. Glacial ages were characterized by significant 13C enrichment, due to the expansion of C4 plants, attributed to an intensification of aridity. Thus, the southwest (SW) summer monsoon, which brings the majority of rainfall to the Central Himalayan southern slopes, would have been weaker. Marine sediment cores from the Indian Ocean and Arabian Sea have demonstrated a weaker SW monsoon during glacial periods, and our results confirm that arid conditions and a weak SW monsoon prevailed in the continental interior of the Central Himalayas during glacial ages. This study provides the first continuous record for the continental interior of paleoenvironmental changes directly influenced by the Indian monsoon.

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