Earliest Eocene cold period and polar amplification - Insights from delta H-2 values of lignin methoxyl groups of mummified wood

Three well-preserved mummified wood specimens have been excavated from three earliest Eocene (similar to 55.5, 55.2 and 53.3 Ma) kimberlite pipes in the subarctic Northwest Territories, Canada (similar to 64 degrees N). Each specimen contained multi-decadal length tree-ring series and allowed measurements of stable hydrogen isotope ratios (delta H-2 values) of the lignin methoxyl groups (commonly used cellulose was largely degraded). We used these delta H-2 signatures for the reconstruction of three representative delta H-2 values of the local precipitation by applying calibrated isotope fractionations to investigate deep-time paleoclimatology. Our reconstructions indicate unprecedented low values for the subarctic early Eocene which, however, show within similar to 2.2 Myr an increasing trend from 206 17, 202 17 to 168 17 parts per thousand. These values were interpreted along with other Arctic, subarctic and mid-latitudinal proxy records of that time period indicating in total a period of low stable hydrogen and oxygen isotope ratios in precipitation (onset between 55.7 and 54.9 Ma and a recovery at 53.3 +/- 0.6 Ma) which is assumed to have been primarily caused by a continental cold period. An increased magnitude of this cold period was noted for our subarctic reconstructions pointing to a polar amplification where surface air temperature changes in the Arctic exceed the global trend (in response to climate forcing). In an attempt to quantify the polar amplification magnitude we estimated Arctic temperature changes using our delta H-2 results in combination with existing relationships between early Eocene temperatures and stable water isotopes. Comparing the Arctic temperature change with a global estimation proposes a polar amplification of magnitude <4. Our estimate for the earliest Eocene shows either agreement or indicates a lower magnitude when compared to previously described Cenozoic polar amplifications commonly ranging between 2 and 4.