<p>Lake Baikal is the world&#8217;s largest (by volume), deepest, and oldest (30-40 Ma) lake. In the catchment, climate varies from arid to semi-arid to arctic-boreal with extreme seasonal and spatial differences in temperature and precipitation<sup>1</sup>. Elevation ranges from 450-3000m, resulting in a large range of geomorphic settings. The catchment has also been affected by periodic Quaternary glaciations<sup>2</sup>. Although the geology of the catchment is diverse and contains igneous, metamorphic and sedimentary rocks of Archean to Cenozoic ages, the most prominent lithologies are granitoids and gneisses with only minor carbonate contributions<sup>1</sup>. Continuous lake sediment cores are available recording the Quaternary glacial cycles, and even dating back into the Miocene. Lake Baikal is therefore a promising site to study variation of silicate rock weathering in both space and time.</p><p>In preparation for paleo-studies, we constrain the present-day budget of the lake with respect to radiogenic weathering tracers (Nd, Pb, and Sr) and meteoric <sup>10</sup>Be/<sup>9</sup>Be isotope ratios. &#160;Nd, Sr, Pb, and their radiogenic isotope systems show different behaviors in Lake Baikal. Sr concentrations in the lake are similar to riverine inputs, reflecting conservative behavior of Sr and resulting in a uniform isotopic composition that is slightly higher than the average of riverine inputs (possibly due to loess inputs<sup>3</sup>). Pb concentrations are higher in the lake than in the major tributaries. The isotopic composition of both lake and rivers point to anthropogenic sources of Pb. In contrast, Nd concentrations in the lake are much lower than in the rivers. Nd isotopic compositions are similar in the central and southern basin but less radiogenic in the northern basin. Both <sup>10</sup>Be and <sup>9</sup>Be concentrations are much lower in Lake Baikal than in its tributaries, possibly indicating removal due to pH induced changes in dissolved-particulate partitioning<sup>4</sup>. This may also explain the contrast in Nd concentrations between rivers and the lake. <sup>10</sup>Be/<sup>9</sup>Be ratios in the lake are slightly elevated compared to riverine &#160;inputs, suggesting a potential role for dust and/or precipitation as a source for <sup>10</sup>Be<sup>5</sup>. We will also compare silicate weathering fluxes derived from meteoric Be isotope ratios with those derived from major element concentrations and riverine discharges.</p><p>Taken together, these results highlight the importance of assessing modern processes at sediment core locations prior to interpreting variation in the past, and the benefits of using a suite of weathering proxies rather than relying on one: while Sr isotopes at any core location record changes to the chemistry of the whole lake (and the processes in its catchment), Be and Nd isotopes are likely biased to the inputs of the nearest rivers.</p><ol><li>Zakharova et al. Chem. Geol.&#160;<strong>214</strong>, 223&#8211;248 (2005).</li>
<li>Karabanov et al. Quat. Res.&#160;<strong>50</strong>, 46&#8211;55 (1998).</li>
<li>Yokoo et al. Chem. Geol.&#160;<strong>204</strong>, 45&#8211;62 (2004).</li>
<li>You et al. Chem. Geol.&#160;<strong>77</strong>, 105&#8211;118 (1989).</li>
<li>Aldahan et al. Geophys. Res. Lett.&#160;<strong>26</strong>, 2885&#8211;2888 (1999).</li>
</ol>
Changes in C<sub>3</sub>/C<sub>4</sub> vegetation in the continental interior of the Central Himalayas associated with monsoonal paleoclimatic changes during the last 600 kyr
