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author Hallenberger, Maximilian
Reuning, Lars
Back, Stefan
Gallagher, Stephen John
Iwatani, Hokuto
Lindhorst, Katja
author_facet Hallenberger, Maximilian
Reuning, Lars
Back, Stefan
Gallagher, Stephen John
Iwatani, Hokuto
Lindhorst, Katja
collection Datos científicos de ciencias marinas y ambientales
contents The North West Shelf of Australia is an extensive tropical carbonate ramp and forms an important template for the interpretation of similar systems in the sedimentary record. Yet, little is known about the development of the distally steepened ramp from the middle to late Quaternary, a period of high frequency glacioeustatic changes in sea level and climate. This research describes core and seismic-reflection data from a mid- to outer ramp transect at the Northwest Shelf. Carbonates occurring within the studied site can be subdivided by color into light and dark sections. These differences are linked to composition and mineralogy, which in turn are related to changes in the sedimentary environment. Based on this relationship, reflectance of visible light (i.e. lightness) can be used as a high-resolution proxy to delineate different facies within the core.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_927013
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Lightness measurement from IODP Site 356-U1461
Hallenberger, Maximilian
Reuning, Lars
Back, Stefan
Gallagher, Stephen John
Iwatani, Hokuto
Lindhorst, Katja
356-U1461A; 356-U1461B; 356-U1461C; APC; Aragonite-needle mud; Australian Shelf; Autoclave piston corer; Color, L*, lightness; Date/Time of event; DEPTH, sediment/rock; Distally steepened ramp; Event label; Exp356; Half-length advanced piston corer; HLAPC; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Latitude of event; Longitude of event; Lowstand shedding; NWS; Ooids; RCD; Rotary core drilling; Spectrophotometer, Ocean Optics USB4000
The North West Shelf of Australia is an extensive tropical carbonate ramp and forms an important template for the interpretation of similar systems in the sedimentary record. Yet, little is known about the development of the distally steepened ramp from the middle to late Quaternary, a period of high frequency glacioeustatic changes in sea level and climate. This research describes core and seismic-reflection data from a mid- to outer ramp transect at the Northwest Shelf. Carbonates occurring within the studied site can be subdivided by color into light and dark sections. These differences are linked to composition and mineralogy, which in turn are related to changes in the sedimentary environment. Based on this relationship, reflectance of visible light (i.e. lightness) can be used as a high-resolution proxy to delineate different facies within the core.
title Lightness measurement from IODP Site 356-U1461
topic 356-U1461A; 356-U1461B; 356-U1461C; APC; Aragonite-needle mud; Australian Shelf; Autoclave piston corer; Color, L*, lightness; Date/Time of event; DEPTH, sediment/rock; Distally steepened ramp; Event label; Exp356; Half-length advanced piston corer; HLAPC; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Latitude of event; Longitude of event; Lowstand shedding; NWS; Ooids; RCD; Rotary core drilling; Spectrophotometer, Ocean Optics USB4000
url https://doi.org/10.1594/PANGAEA.927013