Morpho-tectonic control on the distribution of C3-C4 plants during Late Plio-Pleistocene in the central Himalayan Siwaliks

Abstract

<p>The Siwalik deposits of Himalayan foreland basin (HFB) preserved the Miocene records of the Himalayan tectonics, monsoonal variation and evolution of C<sub>4 </sub>plants. Previous vegetation reconstructions emphasized   the Late Miocene expansion of C<sub>4</sub> plants (ca. 7 Ma) with an implicit assumption that the vegetation thrived in the floodplain of lowland rivers. The coarsening-upward sequence of the Siwalik Group suggests deposition  in an alluvial fan setting in which the Middle and Lower Siwaliks are deposits of distal area whereas the Upper Siwaliks represent proximal areas of the fan. The modern alluvial fans forming in the Himalayan foothills show a significant difference in elevation and vegetational composition between proximal and distal areas. In the HFB, the elevation difference between the proximal and distal areas is expected to be more pronounced due to surface exhumation of the Siwalik deposits. The increased elevation would have had affected the vegetation distribution in the Upper Siwaliks which implies that vegetation  inproximal part of the fan might not represent lowland floodplain. However, the vegetation composition is less understood from the Upper Siwaliks region as conventional proxies are scanty in these younger foreland deposits.</p><p>In the present study, the impact of elevation on vegetation distribution in the HFB is examined from comparatively higher exhumed Late Plio-Pleistocene Siwalik deposits at SuraiKhola (Nepal). The δ<sup>13</sup>C values of bulk soil organic matter (SOM), n-alkane and n-alkanoicacid from the SuraiKholapaleosols suggest most commonly observed expansion of the C<sub>4</sub> plants at ca. 7 Ma, and a unique second phase of expansion of C<sub>3</sub> plants after ca. 3 Ma. The higher δD values in n-alkane and n-alkanoicacid suggest that the climate was drier in last 4 Myr; most likely driven by the onset of the Northern Hemisphere Glaciation (NHG). The growth of C<sub>3</sub> plants was favored due to cool climatic condition induced by higher elevation in the proximal part of the fan. The water-bearing conglomerate units in the Upper Siwaliks helped the C<sub>3 </sub>plants to thrive in a relatively drier climate. Therefore, the higher abundance of C<sub>3</sub> plants in the Upper Siwaliks suggests morpho-tectonic control on vegetation with the possible influence of NHG.</p><p> </p>