Lithium Isotopes as Proxy of Continental Silicate Weathering

Monday, 15 December 2014: 4:00 PM
Xiao-Ming Liu1,2, Christoph Wanner3, Roberta L Rudnick2 and William F McDonough2, (1)Carnegie Inst of Washington, washington DC, DC, United States, (2)Univ Maryland, College Park, MD, United States, (3)Lawrence Berkeley National Laboratory, Earth Sciences Division, Berkeley, CA, United States
Chemical weathering has an important influence on continental crust evolution, as weathering of basalt preferentially removes soluble elements, such as Mg and Ca, and can shift the crust towards more andesitic compositions, thus helping to solve the crustal composition paradox. The isotopic compositions of soluble elements (e.g., Li and Mg) provide a monitor of chemical weathering of the continents through time.

Here we evaluate the factors influencing the abundance, [Li], and isotopic composition of riverine Li delivered to the oceans through analyses and modeling of [Li] and d7Li in streams and groundwaters draining a single continental lithology, the Columbia River Basalts (CRBs). The streams were sampled in different climate zones that lie on the dry and wet sides of the Cascades Mountains, and during two different seasons (summer and late winter) in order to evaluate climatic and seasonal influences on Li isotopes in rivers. Dissolved Li (δ7Li = +9.3 to +30.4) is systematically heavier than that of fresh or weathered CRBs, suspended loads (-5.9 to -0.3), and shallow groundwaters (+6.7 to +9.4). Continued isotopic fractionation between stream water and suspended and/or bed loads has a major influence on riverine δ7Li as indicated by the heavier Li in streams, compared to the shallow groundwaters that feed them. Seasonal δ7Li variation is observed only for streams west of the Cascades, where the difference in precipitation rate between the seasons is greatest. Reactive transport model simulations reveal that riverine δ7Li is strongly controlled by subsurface residence times and Li isotope fractionation occurring within rivers. The varying residence times for groundwaters feeding the western streams in summer (long residence times, higher δ7Li, greater weathering) and winter (short residence times, lower δ7Li, less weathering) explains the observed seasonal variations. A global, negative correlation between δ7Li and Li/Na for streams and rivers draining basaltic catchments reflects the overall transport time, hence the amount of silicate weathering. Based on our results, the increase of δ7Li in seawater during the Cenozoic is unlikely related to changing climate, but may reflect mountain building giving rise to increased silicate weathering.