| polarity-reversal horizon | Either a single, clearly definable surface or a thin body of strata constituting a transitional interval across which a change in magnetic polarity is recorded (north american stratigraphic code, ... |
| acme zone | Equivalent to abundance zone (see section 7.d.6.c). |
| flood zone | Equivalent to abundance zone (see section 7.d.6.c). |
| peak zone | Equivalent to abundance zone (see section 7.d.6.c). |
| time-rock unit | Equivalent to chronostratigraphic unit. |
| time-stratigraphic unit | Equivalent to chronostratigraphic unit. 141 |
| time-stratigraphy | Equivalent to chronostratigraphy. 142 |
| chronotaxy | Equivalent to chronotaxis as originally proposed by henbest (1952, p. 310). |
| overlap zone | Equivalent to concurrent-range zone (see section 7.d.2.b.iii). |
| range-overlap zone | Equivalent to concurrent-range zone (see section 7.d.2.b.iii). |
| faunizonite | Equivalent to faunizone (henningsmoen, 1961, p. 69). |
| florizonite | Equivalent to florizone (henningsmoen, 1961, p. 69). |
| reference section | Equivalent to hypostratotype (see section 4.b.7.e). |
| auxiliary reference section | Equivalent to hypostratotype (see section 4.b.7.e). b band. a thin stratum with a distinctive lithology or color that is useful in correlating strata (see calkins, 1941). |
| biointerval zone | Equivalent to interval zone (international stratigraphic guide, 1976, p. 60). |
| interbiohorizon zone | Equivalent to interval zone (international stratigraphic guide, 1976, p. 60). |
| morphogenetic zone | Equivalent to lineage zone (see section 7.d.4.c). |
| phylogenetic zone | Equivalent to lineage zone (see section 7.d.4.c). |
| evolutionary zone | Equivalent to lineage zone (see section 7.d.4.c). f |
| rock-stratigraphic unit | Equivalent to lithostratigraphic unit. |
| rock unit | Equivalent to lithostratigraphic unit. s |
| rock-stratigraphy | Equivalent to lithostratrigraphy. |
| soil-stratigraphic unit | Equivalent to pedostratigraphic unit. span. a unit o f low rank in the hierarchy o f diachronic units (north american stratigraphic code, 1983, p. 870). |
| stratic unit | Equivalent to stratigraphic unit (henningsmoen, 1961, p. 63). |
| type section | Equivalent to stratotype (see section 4.b.1). u |
| wagone | Etal., 1987, p. 11). b. the study of genetically related facies within a framework of chronostratigraphically significant surfaces (van wagoner et al., 1990, p. 1). |
| ethnostratigraphy | Ethnostratigraphic classification. the stratigraphic classification into units characterized by their content of archaeological artefacts; archaeological stratigraphy (guide to archaeostratigraphi... |
| reworked fossils | Fossils from rocks of one age that have been eroded, transported, and redeposited in sediments of a younger age (see section 7.b.3). |
| introduced fossils | Fossils originally in younger rocks later introduced in any one of several ways into the older rocks in which they are now found (see section 7.b.4). |
| standar | Global chronostratigraphic (geochronologic) scale. the hierarchy of chronostratigraphic units (and their equivalent geochronologic units) of worldwide scope which will serve as a standard scale of... |
| equivalent to the sequence o | Mitchum, vail, and thompson (1977). |
| in the case of stratigraphic units composed o | Nonlayered igneous or metamorphic rock bodies, the type locality is the specific geographic locality where the unit was originally defined and named (see section 4.b.5). |
| component-stratotype | One of several specified intervals of strata making a composite-stratotype (see section 4.b.4). |
| correspondence in age and chronostratigraphi | Position between two stratigraphic sections (see sections 3.a.9 and 9.1). |
| topostratigraphy | Preliminary or introductory stratigraphy, including lithostratigraphy and biostratigraphy. |
| biodatum | See biohorizon. |
| biocorrelation | See biostratigraphic correlation. |
| biolevel | See biostratigraphic horizon. |
| chronocorrelation | See chronostratigraphic correlation. |
| chronostratigraphic zone | See chronozone. |
| coincident-range zone | See concurrent-range zone. 114 |
| chronometric unit | See geochronometric unit. |
| marker point | See global boundary stratotype section and point. |
| depositional holosome | See holosome. |
| hiatal holosome | See holosome. |
| geohydrologic unit | See hydrostratigraphic unit. |
| infiltrated fossils | See introduced fossils. |
| lithocorrelation | See lithostratigraphic correlation. |
| chronotaxis | Similarity in sequence with respect to age (henbest, 1952, p. 310). |
| geologica | - Society o f london, 1967, p. 85). b. a biozone characterized by one taxon o f a lineage, in such a way that the precurdownloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/374...
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| commission o | Stratigraphic nomenclature, 1957, report 5, p. 1884). n |
| the term has subsequently been used for | Stratigraphic unit, a part o f a stratigraphic section, a particular kind o f sediment or rock, a body o f uniform sediments formed by persistence o f the depositional environment, and, in an inta... |
| independent units | Stratigraphic units that do not meet each other (henningsmoen, 1961, p. 66). |
| parastratigraphy | Supplemental stratigraphy based on fossils other than those governing the prevalent orthostratigraphy (schindewolf, 1957, p. 397). |
| formal stratigraphic terminology | Terminology applied to stratigraphic units (formal stratigraphic units) that is properly defined according to an established or conventionally agreed scheme of classification (see section 3.a.5.a)... |
| datum level or datum plane | The base or top of a range of fossils that can be correlated in sections over a wide area (see section 7.c.4). |
| chronosome | The body o f rock enclosed between two markers that may approximate isochronous surfaces and so define the upper and lower limits o f a single period o f deposition within a basin. it is a special... |
| total-range zone | The body o f strata that comprises the complete horizontal and vertical range o f occurrence o f a specified fossil group (report o f the stratigraphical code sub-committee, geological society o f... |
| taxon-range zone | The body of strata representing the known range of occurrence (stratigraphic and geographic) of specimens of a certain taxon (species, genus, family, etc.) (see section 7.d.2.a). |
| range zone | The body of strata representing the known stratigraphic and geographic range of occurrences of any selected element or elements of the assemblage of fossils present in a stratigraphic sequence (se... |
| lithostratigraphy | The element of stratigraphy that deals with the description and systematic organization of the rocks of the earth`s crust into distinctive 127 named units based on the lithologic character of the ... |
| magnetostratigraphy | The element of stratigraphy that deals with the magnetic characteristics of rock units (see section 8.b.1). |
| chronostratigraphy | The element of stratigraphy that deals with the relative time relations and ages of rock bodies (see section 9.b.1). |
| alloformation | The fundamental allostratigraphic unit (see allostratigraphic unit). |
| diachron | The fundamental and nonhierarchical diachronic unit (north american |
| lithodeme | The fundamental unit in lithodemic classification; a body o f intrusive, pervasively deformed, or highly metamorphosed rock, generally non-tabular and lacking primary depositional structures, and ... |
| facies evolution | The gradual change o f facies in time, indicating gradually changing sedimentation conditions (teichert, 1958b, p. 2723). |
| lapout | The lateral termination o f strata at their depositional pinchout. lapout may occur at the upper boundary o f a sequence, where it is called toplap, or at the lower boundary, where it is called on... седиментационное выклинивание пластов; |
| holostratic unit | The local part o f a stratic unit (henningsmoen, 1961, p. 67). |
| topostratic unit | The local part o f a stratic unit, a “local unit” (henningsmoen, 1961, p. 67). |
| magnetostratigraphic polarity classification | The organization of rock bodies into units based on changes in the polarity of their remanent magnetization, related to reversals in the polarity of the earth’s magnetic field (see section 8.b.4).... |
| magnetostratigraphic classification | The organization of rock bodies into units based on differences in magnetic character (see section 8.b.2). |
| lithostratigraphic classification | The organization of rock bodies into units on the basis of their lithologic properties (see section 5.b.2). |
| chronostratigraphic classification | The organization of the rocks of the earth`s crust into units on the basis of their age or time of formation (see section 9.b.2). |
| holostratotype | The original stratotype designated by the original author at the time of proposing a stratigraphic unit or boundary (see section 4.b.7.a). |
| syn-biotope | The overlap area of the auto-biotopes o f two or more systematic units (van |
| stratigraphic leakage | The process whereby sediments and (or) fossils o f a younger age are deposited within or under older rocks. the result or product o f the process of stratigraphic leakage is stratigraphic leak (fo... |
