Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1)

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Main Authors: Egger, Hans, Brückl, Ewald
Format: Dataset Open Access
Language:en
Published: PANGAEA 2007
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author Egger, Hans
Brückl, Ewald
author_facet Egger, Hans
Brückl, Ewald
collection Datos científicos de ciencias marinas y ambientales
contents 23 layers of altered volcanic ash (bentonites) originating from the North Atlantic Igneous Province have been recorded in early Eocene deposits of the Austrian Alps, about 1,900 km away from the source area. The Austrian bentonites are distal equivalents of the ''main ash-phase'' in Denmark and the North Sea basin. We have calculated the total eruption volume of this series as 21,000 km**3, which occurred in 600,000 years. The most powerful single eruption of this series took place 54.0 million years ago (Ma) and ejected ca. 1,200 km**3 of ash material, which makes it one of the largest basaltic pyroclastic eruptions in geological history. The clustering of eruptions must have significantly affected the incoming solar radiation in the early Eocene by the continuous production of stratospheric dust and aerosol clouds. This hypothesis is corroborated by oxygen isotope values, which indicate a global decrease of sea surface temperatures between 1 and 2 C during this major phase of explosive volcanism.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_670359
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1)
Egger, Hans
Brückl, Ewald
Area/locality; Denmark, Jutland; Fur_island; HAND; Isopach area, square root; LATITUDE; Layer thickness; Limfjorden; LONGITUDE; Paleolatitude; Paleolongitude; Sampling by hand
23 layers of altered volcanic ash (bentonites) originating from the North Atlantic Igneous Province have been recorded in early Eocene deposits of the Austrian Alps, about 1,900 km away from the source area. The Austrian bentonites are distal equivalents of the ''main ash-phase'' in Denmark and the North Sea basin. We have calculated the total eruption volume of this series as 21,000 km**3, which occurred in 600,000 years. The most powerful single eruption of this series took place 54.0 million years ago (Ma) and ejected ca. 1,200 km**3 of ash material, which makes it one of the largest basaltic pyroclastic eruptions in geological history. The clustering of eruptions must have significantly affected the incoming solar radiation in the early Eocene by the continuous production of stratospheric dust and aerosol clouds. This hypothesis is corroborated by oxygen isotope values, which indicate a global decrease of sea surface temperatures between 1 and 2 C during this major phase of explosive volcanism.
title Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1)
topic Area/locality; Denmark, Jutland; Fur_island; HAND; Isopach area, square root; LATITUDE; Layer thickness; Limfjorden; LONGITUDE; Paleolatitude; Paleolongitude; Sampling by hand
url https://doi.org/10.1594/PANGAEA.670359