2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)

Paper No. 251-1
Presentation Time: 1:00 PM

SEASONAL TEMPERATURE AND PRECIPITATION AMOUNT RECORDED IN MONTHLY OXYGEN ISOTOPE MEASUREMENTS OF METEORIC WATER


SCHUBERT, Brian A., School of Geosciences, University of Louisiana at Lafayette, 611 McKinley St 44530, Hamilton Hall #323, Lafayette, LA 70504 and JAHREN, A. Hope, Geology and Geophysics, University of Hawaii, 1680 East-West Road, POST 701, Honolulu, HI 96822

The oxygen isotope composition of meteoric water (δ18OMW) is commonly reconstructed from a wide variety of substrates in order to reconstruct mean annual climate at a given site. These reconstructions are based on robust relationships showing that temperature, latitude, altitude, and precipitation all affect δ18OMW values. However, a quantitative relationship to assess how seasonal climate affects seasonal changes in δ18OMW (Δδ18OMW) has not been determined. Here we use the International Atomic Energy Agency’s Global Network of Isotopes in Precipitation database to produce a global relationship relating seasonal climate (i.e., temperature and precipitation) to Δδ18OMW. We include in our analysis 365 stations that reported a complete suite of monthly temperature, precipitation, and δ18OMW data. From these data, we produced a global relationship between average monthly temperature (T) and average monthly δ18OMW value (R = 0.80, n = 4312) and identified a non-linear δ18OMW/T gradient that decreases with increasing temperature. This relationship was able to explain most of the variability in Δδ18OMW for the sites located >37o from the equator (R = 0.88, n = 219), but was a poor-predictor of Δδ18OMW at all other sites (R = 0.30, n = 146). By incorporating the effect of changes in seasonal precipitation amount (which is greatest in the tropics) to our relationship, we hoped to reconcile the poor fit observed within our low latitude sites. Towards this, we calculated a δ18OMW depletion rate = 0.0082 ‰/mm, that when applied to all 365 sites, allowed us to predict the Δδ18OMW value for all sites through knowledge of seasonal changes in temperature and precipitation amount (R = 0.83, n = 365). The wide applicability of this relationship to diverse climates and geographic locations makes it particularly relevant towards reconstructing seasonal climate from geologic substrates containing seasonal δ18OMW information (e.g., tree-rings, teeth, speleothems).