Maximum marine flooding events constitute regional chronostratigraphic correlative surfaces in foreland basins dominated by continental sedimentary fill, such as in the Colombian Llanos Basin.
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The separation between the group and the stage was made in the second half of the 20th century, when stratigraphers saw the need to distinguish between lithostratigraphic and chronostratigraphic names.
Andean Geology accepts articles dealing with systematic Paleontology only if their main focus is the chronostratigraphic, paleoecologic and/or paleogeographic importance of the taxa described therein.
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The identification and characterisation of these significant volcanic events provide new constraints into regional Holocene geological and archaeological records, and offer extensive regional chronostratigraphic markers over a wide geographical area of South America.
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Latest Era Or Highest Erathem: The full name of the latest possible geochronologic era or highest chronostratigraphic erathem attributable to the stratigraphic horizon from which the cataloged item was collected.
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The full name of the earliest possible geochronologic age or lowest chronostratigraphic stage attributable to the stratigraphic horizon from which the cataloged item was collected.
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Latest Age Or Highest Stage: The full name of the latest possible geochronologic age or highest chronostratigraphic stage attributable to the stratigraphic horizon from which the cataloged item was collected.
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Chronological results, along with the chronostratigraphic study of the sites has allowed us to relate the build-up of the 13 identified lithostratigraphic units with different climatic stages.
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The last radiocarbon dates from the Solutrean of La Cueva de Ambrosio allow the clarification of its position in the Upper Pleistocene chronostratigraphic scale.
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The very good correlation with the deep-sea oxygen isotope record, which includes the development of an accurate astronomical time scale, allows a detailed chronostratigraphical subdivision of the loess-paleosol sequence in Karamaydan down to the substage level, which therefore should be regarded as a key sequence in the temperate climatic belt of the Northern Hemisphere for reconstructing the climate history of the Brunhes epoch.
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The chronostratigraphic sequence of the Alto de la Cruz site covers a chronological period between the Bronze Age (around 1100 BC) and the second Iron Age (around 350 BC), and is crucial for studying the transition and the continuity of settlement between the indigenous substrate of the middle-late Bronze Age in the Ebro valley, and the communities that settled in the area at the end of the Bronze Age.
For certain subdivisions of the scale used "inferior" and "superior" if referring to chronostratigraphic units units (rock bodies) or "early" and "late" if it refers to geochronologic units (time).
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The succession of these horizons and other ones already defined in previous papers, are associated to the Andean chronostratigraphic scale which is then used for fine time-correlation between sections of several localities of the Neuquén-Mendoza Basin where a number of them could be recognized by means of their characteristic ammonite assemblages.
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The identification and characterisation of these significant volcanic events provide new constraints into regional Holocene geological and archaeological records, and offer extensive regional chronostratigraphic markers over a wide Insights to the Holocene eruptive deposits in the southern Puna and adjacent regions.
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These are the units that are established chronostratigraphic scale divisions standard for Phanerozoic (and Precambrian Ediacaran). Are used as support material.
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