Infilling of the Canche Estuary (eastern English Channel, France): Insight from benthic foraminifera and historical pictures
Fabio FrancescangeliMélanie PortelaÉric ChâteletGabriel BillonThorbjørn Joest AndersenVincent M. P. BouchetAlain Trentesaux
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Salt marsh
Subfossil
Radiometric dating
Paleolimnology
Chronostratigraphy
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Paleolimnology
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Paleoclimatology
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Abstract This chapter reviews the progress made between the years 1965 and 2000 in temporal techniques and their importance for the study of landforms. The chapter begins with discussion of advances in chronostratigraphy and of the important contributions to geomorphology that came from palaeoenvironmental reconstruction, notably through the study of marine sediments and ice cores. A more detailed discussion then follows of developments and advances in dating methods, grouped by radiometric and radiometric-related, incremental, age-equivalent markers, and relative, with emphasis on the ways in which the new techniques opened up new avenues in the study of landforms.
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A K-Ar age was determined for the Kn-1 Tuff in the Miocene marine sequence of the Kawadani section in the Boso Peninsula, central Japan. The weighted-mean age of 14.95±0.24Ma (±σ error) was calculated from two ages on Kn-1 biotite (14.96±0.34Ma and 14.93±0.34Ma). Combining with previously reported radiometric ages of other tuff layers, the established chronostratigraphy based on the radiometric dating indicates decline of the sedimentation rate between the Kn-3 Tuff in the upper part of the Kinone Formation and the Am-4 Tuff in the lowest part of the Amatsu Formation. The previously established biostratigraphy of microfossils is almost consistent with the chronostratigraphy of radiometric ages, while only the age of the last occurrence of Eucyrtidium asanoi (radiolaria) is suggested to be younger (ca. 12.2-12.7Ma) than the previous estimation (13.56-13.85Ma) by Morley and Nigrini (1995).
Chronostratigraphy
Radiometric dating
Peninsula
Sequence (biology)
Absolute dating
K–Ar dating
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This report describes the location and character of ten Carboniferous-Permian igneous rock
samples from the Midland Valley of Scotland and the results of 40Ar/39Ar step-heating
experiments on nine of the samples to obtain the radiometric age of eruption or emplacement of
the rock. The quality of the new radiometric ages are discussed along with their integration with
the chronostratigraphy, lithostratigraphy and biostratigraphy of the Midland Valley of Scotland.
Chronostratigraphy
Radiometric dating
Lithostratigraphy
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Arctic ecology
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Paleoclimatology
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Paleoecology
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