Mathematical Bases for Formulation of Biostratigraphic Methods

  • SHIONO Kiyoji
    Department of Geosciences, Faculty of Science, Osaka City University
  • YAMAGUCHI Kumiko
    Department of Geosciences, Faculty of Science, Osaka City University

Bibliographic Information

Other Title
  • 生層序学的方法を形式表現するための数学的基礎
  • 生層序学的方法を形式表現するための数学的基礎--古生物の生存期間と年代区分
  • セイソウジョガクテキ ホウホウ オ ケイシキ ヒョウゲンスル タメ ノ スウガ
  • ―古生物の生存期間と年代区分―
  • —Life Interval of Fossil and Geological Age—

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Abstract

We propose a mathematical framework for formulation of biostratigraphic methods based on two order relations ≤__??_ and <<_??_ on a set whose members are intervals of a totally ordered set (A, ≤) defined by: [a, b] ≤_??_ [a′, b′] iffaa′and b≤b′, and [a, b] <<_??_ [a′, b′] iffba′or [a, b] = [a′, b′] .Let Σ0 be a set whose members are individuals of animals and plants which lived within an intervalT, and S0be a partition ofΣ0. An element ofS0is called here“an individual class”.We define a range of an individual class σ, denoted by τ (σ), by union of life intervals of all individuals in σ. This framework enables us to formulate easily several basic concepts. A combination of individual classes which lived together at a timetis given bys (t) = {α|t∈τ (α) } .A range in which the same combination of individual classes lived together is expressed by an equivalence class relative to an equivalence relation-such thatp-qiffs (p) =s (q) .It is possible to order individual classes based on a relation κ such that α κ β iff τ (α) ≤_??_τ (β) . Further we discuss the details of time classification based on a setSwhich satisfies three assumptions (1) Sis a subset ofS0such that τ (σ) is an interval ofTfor all σ∈S, (2) (S, κ) is a total ordering, and (3) s (t) is a non-empty set for alltT. The results suggest that the proposed mathematical framework is useful to formulate basic concepts of biostratigraphy.

Journal

  • Geoinformatics

    Geoinformatics 8 (4), 227-237, 1997

    Japan Society of Geoinformatics

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