Isotopes in Quaternary Paleoenvironmental Reconstruction

This special issue emerged from a 2002 meeting on “Isotopes in Quaternary Palaeoenvironmental reconstruction” (ISOPAL) that was one of a series of PAGES sponsored workshops contributing to the Pole–Equator–Pole (PEP III) transect.

> Palaeo-climate reconstruction from stable isotope variations in speleothems: a review [p.901]
McDermott F

> Constraints on hydrological and paleotemperature variations in the Eastern Mediterranean region in the last 140 ka given by the δD values of speleothem fluid inclusions [p.919]
McGarry S, Bar-Matthews M, Matthews A, Vaks A, Schilman B & Ayalon A

> Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually laminated speleothems from Southern Oman [p.935]
Fleitmann D, Burns SJ, Neff U, Mudelsee M, Mangini A & Matter A

> 230Th/234U dating of Holocene tufas: possibilities and problems [p.947]
Garnett ER, Gilmour MA, Rowe PJ, Andrews JE & Preece RC

> Bone as a stable isotope archive for local climatic information [p.959]
Hedges REM, Stevens RE & Richards MP

> Using mammal tooth phosphate with freshwater carbonate and phosphate palaeoproxies to obtain mean paleotemperatures [p.967]
Grimes ST, Mattey DP, Collinson ME & Hooker JJ

> Carbon and nitrogen stable isotope analysis of northwest European horse bone and tooth collagen, 40,000 BP–present: Palaeoclimatic interpretations [p.977]
Stevens RE & Hedges REM