A horizontal core through a large, standing, stalagmite in Carlsbad Caverns National Park, New Mexico, USA, provides a radiometrically dated record of wetter glacial stages and drier interglacial stages over the last 560. kyr. The stalagmite, the Texas Toothpick, is about 7. m tall and about 3. m wide at its base. Two cores through the stalagmite reveal five distinct matching layers, and the best estimates from twenty U-Th ages indicate that those layers were deposited during MIS 6, 8, 10, 12, and 14, the five glacial periods ending with the Penultimate Glacial Maximum (PGM). Stable isotope data, measurements of remanent magnetism, and petrographic observations combine to suggest that conditions during glacials, the periods in which deposition took place, were significantly wetter than today. On the other hand, the stalagmite's hiatuses seemingly represent conditions during interglacials similar to or drier than today. These results combine with modern climatological observations to suggest 100-kyr-scale alternation between wetter conditions with an increased proportion of winter rainfall from a Pacific source during glacials to drier conditions with largely summer rainfall derived from the Gulf of Mexico during interglacials. The length and continuity of the results confirm that the pattern of wetter glacials and drier interglacials, known previously from studies isolated in time, existed across all of at least the last six glacial cycles. Simple monotonic extrapolation of these findings from cooler wetter glacials of the past and warmer drier interglacials like the present to a warmer climate expected in the coming century suggests that groundwater in the already
|Original language||English (US)|
|Number of pages||11|
|Journal||Palaeogeography, Palaeoclimatology, Palaeoecology|
|State||Published - Nov 15 2015|
Bibliographical noteFunding Information:
This work was partially supported by Grant 2577-82 from the National Geographic Society to BBE and GAB and by Grant NSF 1103320 from the U.S. National Science Foundation to RLE. We are grateful to the National Park Service for allowing the drilling of the two speleothems. Special thanks go to Ron Kerbo, Cave Specialist for the Park Service, for his many hours of help on this project. Also gratefully acknowledged for many hours help in the cave during sampling are Mark Earley and Suzanne, Amber, Robin, and Richard Ellwood. The late Victor Schmidt is gratefully acknowledged for allowing use of his cryogenic magnetometer for the RM measurements. The manuscript was improved by the comments of three PPP reviewers, one of whom generated Table 3 .
© 2015 Elsevier B.V..