MATHEMATICAL AND IMAGE ANALYSIS OF STROMATOLITE MORPHOGENESIS

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dc.contributor.author Batchelor M.T.
dc.contributor.author Burne R.V.
dc.contributor.author Henry B.I.
dc.contributor.author Watt S.D.
dc.date.accessioned 2022-02-04T03:58:43Z
dc.date.available 2022-02-04T03:58:43Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=13938673
dc.identifier.citation Mathematical Geology, 2003, 35, 7, 789-803
dc.identifier.issn 0882-8121
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/34929
dc.description.abstract Stromatolites are internally laminated organosedimentary structures that result from the environmental interactions of Benthic Microbial Communities. They have been traditionally described and classified either by quasi-Linnean taxonomic systems or by morphometric schemes. Neither of these approaches has proved entirely satisfactory. The application of the mathematics of evolving surfaces provides a promising alternative for the modelling and classification of stromatolites in terms of their morphogenesis. The suggestion of Grotzinger and Rothman that stromatolite-growth in general could be attributed to a combination of four processes that constitute the variables of the Kardar–Parisi–Zhang (KPZ) equation has been analyzed and found to be an oversimplification. While some stromatolites can be characterized in this way, because of local growth effects, the majority of stromatolite forms exhibit nonlocal growth characteristic of Laplacian growth. Work is being undertaken to model such growth.
dc.subject stromatolites
dc.subject morphogenesis
dc.subject KPZ equation
dc.subject Laplacian growth
dc.title MATHEMATICAL AND IMAGE ANALYSIS OF STROMATOLITE MORPHOGENESIS
dc.type Статья


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