Philosophical Transactions of the Royal Society B: Biological Sciences

Studies in the vegetational history of Scotland. IV. Pine stumps in Scottish blanket peats

Regional pollen stratigraphy, identifiable and well constrained

Welten, M. 1982. Vegetationsgeschichtliche Untersuchungen in den westlichen Schweizer Alpen: Bern-Wallis. Denkschriften der Schweizerischen Naturforschenden Gesellschaft, Vol. 95. DSNG 95. Textheft 104 pp., Diagrammheft 37 diagrams.

Denkschriften der Schweizerischen Naturforschenden Gesellschaft

Vegetationsgeschichtliche Untersuchungen in den westlichen Schweizer Alpen: Bern-Wallis

Mariscal, B. 1993. Variacion de la vegetacion Holocena (4300-280 BP) de Cantabria a traves del analisis polinico de la turbera del Alsa. Estudios Geologicos. Museo Nacional Ciencias Naturales. CSIC.

Variacion de la vegetacion Holocena (4300-280 BP) de Cantabria a traves del analisis polinico de la turbera del Alsa

Zatyko, C.S., I. Juhasz, and P. Suemegi. 2007. Environmental archaeology in Transdanubia. Budapest: Archaeological Institute of the Hungarian Academy of Sciences. Varia archaeologica Hungarica 20(2007) 391p.

De Valk, E.J. 1981. Late Holocene and present vegetation of the Kastelberg (Vosges, France). Ph.D. Dissertation. University of Utrecht, Utrecht, The Netherlands.

Late Holocene and present vegetation of the Kastelberg (Vosges, France)

chronology data missing; the response of d180L to the temperature controlled variations in d18Op will be characteristic for each lake and, therefore, must be evaluated by hydrological investigations for any lake used for paleoclimatic reconstructions...d18OL of Lake Ammersee proved to be sensitive to mean air temperature variations with periods higher than 10 years and amplitudes larger than 0.3 Kelvin.

CARBO Kiel MAT 251 CO2 preparation and massspectrometer system

Check symbols in isotopeInterpretation2_coefficient. Has isotopeInterpretation3_basis but no other details. lake residence time move to sensorIntegration?-BK

Mean d1880c. of replicates from 15 individuals (instars 6 and 7) is 4.60% for the winter 19921993 (15~~0, = 9.5%0) and 4.68% for the winter 19931994 (6permil*OL = 9.50, Table 1). Actual d180c. in both seasons is enriched compared to the isotopic composition of a theoretical calcite formed isotopic equilibrium ( d180eq). The difference is +2.3 2 O.l%o to a 6permil80, calculated using the fractionation factors given by Friedman and OpermilNeil ( 1977) and exactly matches the vital offsets for adults and juveniles of these species found during a oneyear calibration study in Ammersee and Starnberger See, which will be presented and discussed elsewhere.