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• W2053997986 abstract "Framework (sensu stricto) is a concept originally relating to modern reefs and is defined by structural, ecological and sedimentological criteria. However, in the geological literature the term `framework' has come to be applied to almost any organically influenced in situ accumulation, including non-calcareous, non-rigid facies associated with sea grasses. This drastic departure from the original meaning is misleading and scientifically unhelpful. The concept of wave resistance is integral to that of framework, but in the geological record it is not easy to evaluate and the term may be of little comparative use between reef environments. It is suggested that the term growth fabric be generally applied as a descriptive term for the presence of aggregated in situ corals (or other organisms) in growth position within a facies. The term growth fabric should be used as an alternative to `framework' as a purely descriptive term. The term framework should be restricted to its original definition and used only where the criteria for framework can be clearly demonstrated. Two end-member types of scleractinian growth fabric genesis are recognised, termed superstratal and constratal (terms adapted from Gili, E., Masse, J.P., Skelton, P.W., 1995. Rudists as gregarious sediment-dwellers, not reef-builders, on Cretaceous carbonate platforms. Palaeogeogr., Palaeoclimatol., Palaeoecol. 118, 245–267). In a superstratal growth fabric, the constituent organisms collectively projected decimetres to metres above the substratum creating positive topographic relief. In contrast, constratal growth is where vertical organic accretion occurred at a similar rate to sediment accumulation; hence the majority of the skeletal material remained continuously embedded in the sediments, and only a small proportion of the skeleton projected (centimetres) above the sediment surface. The architectural, palaeoecological, sedimentological and diagenetic implications of different types of growth fabric genesis is discussed. A review of the classification of reef fabrics suggests that there is currently no adequate system to describe fossil scleractinian growth fabrics. The most commonly used classification of reefal fabrics is that of Embry and Klovan (1971). [Embry, A.F., Klovan, J.E., 1971. A Late Devonian reef tract on northeastern Banks Island, Northwest Territories. Bull. Can. Pet. Geol. 33, 730–781.] There are a number of shortcomings in this scheme which may be grouped into three categories: (1) the interpretative nature of the classification; (2) problems in interpreting biological effect from form; and (3) insufficient categories to adequately describe Mesozoic and Cenozoic growth fabrics. Moreover, there appears to be a lack of a standardised nomenclature for growth fabrics which has hindered meaningful comparisons of scleractinian growth fabrics through time and space. A descriptive system based on a modification and expansion of the Embry and Klovan system (1971) is proposed and a revised nomenclature for growth fabrics presented. The system is designed to be flexible in its application — it can be used simply to describe a growth fabric, or, through the use of genetic and non-genetic modifiers, to imply types of reef-building processes and growth fabric heterogeneity. Although the concepts and terminology discussed in this paper relate to scleractinian growth fabric, they are equally applicable to fabrics comprising other organisms." @default.
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• W2053997986 date "1998-06-01" @default.
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• W2053997986 title "The descriptive nomenclature and classification of growth fabrics in fossil scleractinian reefs" @default.
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• W2053997986 doi "https://doi.org/10.1016/s0037-0738(98)00011-6" @default.
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