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Comment on: Paleoclimatic inference from stable isotope profiles of accretionary biogenic hardparts: a quantitative approach to the evaluation of incomplete data, by Wilkinson, B.H., Ivany, L.C., 2002. Palaeogeogr. Palaeocl. Palaeoecol. 185, 95-114
De Ridder, F.; de Brauwere, A.; Pintelon, R.; Schoukens, J.; Dehairs, F.A.; Baeyens, W.F.J.; Wilkinson, B.H. (2007). Comment on: Paleoclimatic inference from stable isotope profiles of accretionary biogenic hardparts: a quantitative approach to the evaluation of incomplete data, by Wilkinson, B.H., Ivany, L.C., 2002. Palaeogeogr. Palaeocl. Palaeoecol. 185, 95-114. Palaeogeogr. Palaeoclimatol. Palaeoecol. 248(3-4): 473-476
In: Palaeogeography, Palaeoclimatology, Palaeoecology. Elsevier: Amsterdam; Tokyo; Oxford; New York. ISSN 0031-0182; e-ISSN 1872-616X, meer
Peer reviewed article  

Beschikbaar in  Auteurs 
    VLIZ: Open Repository 132201 [ OMA ]

Trefwoorden
    Accretion
    Climate > Palaeoclimate
    Materials > Biogenic material
    Periodicity > Seasonality
    Marien

Auteurs  Top 
  • De Ridder, F., meer
  • de Brauwere, A., meer
  • Pintelon, R.
  • Schoukens, J.
  • Dehairs, F.A., meer
  • Baeyens, W.F.J., meer
  • Wilkinson, B.H.

Abstract
    The time base reconstruction method proposed by Wilkinson and Ivany [Paleoclimatic inference from stable isotope profiles of accretionary biogenic hardparts: a quantitative approach to the evaluation of incomplete data. Palaeogeogr. Palaeocl. Palaeoecol. 185 (2002), 95-114] can be further refined. They have shown that variations in accretion rate can be reconstructed from variations in the period of the measured signal. Here, it is shown that such variations influence not only the period, but also the phase of the signal. So, a refined estimator for the time base is constructed, which takes both period and phase variations into account.

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