Relation of subtropical Atlantic temperature, high-latitude ice rafting, deep water formation, and European climate 130,000-60,000 years ago
Lehman, S.J.; Sachs, J.P.; Crotwell, A.M.; Keigwin, L.D.; Boyle, E.A.
Younger Dryas readvance in Squamish river valley, southern Coast mountains, British Columbia
Friele, P.A.; Clague, J.J.
Raised marine sequences of Lanzarote and Fuerteventura revisited-a reappraisal of relative sea-level changes and vertical movements in the eastern Canary Islands during the Quaternary
Zazo, C.; Goy, J.L.; Hillaire-Marcel, C.; Gillot, P.; Soler, V.; Gonzalez, J.A.; Dabrio, C.J.; Ghaleb, B.
Patterns and processes of Late Quaternary environmental change in a montane region of southwestern Europe
Patterns and causes of millennial-scale climate change in the Pacific Northwest during Marine Isotope Stages 2 and 3
Grigg, L.D.; Whitlock, C.
Last deglacial sea-surface temperature evolution in the Southeast Pacific compared to climate changes on the South American continent
Kim J.-H.; Schneider, R.R.; Hebbeln, D.; Muller, P.J.; Wefer, G.
Quantitative pollen-based climate reconstruction in central Japan: application to surface and Late Quaternary spectra
Nakagawa, T.; Tarasov, P.E.; Nishida, K.; Gotanda, K.; Yasuda, Y.
Comment on ''Formation of large beaches in an area of rapid differential isostatic rebound: the three-outlet control of Lake Agassiz'' by J.T. Teller
Reply to the comment by P.F. Karrow