Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1)
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''...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.670359 2023-05-15T17:33:46+02:00 Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) Egger, Hans Brückl, Ewald MEDIAN LATITUDE: 8.473333 * MEDIAN LONGITUDE: 54.806667 * SOUTH-BOUND LATITUDE: -13.400000 * WEST-BOUND LONGITUDE: 47.700000 * NORTH-BOUND LATITUDE: 13.000000 * EAST-BOUND LONGITUDE: 56.900000 2007-11-29 text/tab-separated-values, 75 data points https://doi.pangaea.de/10.1594/PANGAEA.670359 https://doi.org/10.1594/PANGAEA.670359 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.670359 https://doi.org/10.1594/PANGAEA.670359 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Egger, Hans; Brückl, Ewald (2006): Gigantic volcanic eruptions and climatic change in the early Eocene. International Journal of Earth Sciences, 95, 1065-1070, https://doi.org/10.1007/s00531-006-0085-7 Area/locality Denmark Jutland Fur_island HAND Isopach area square root LATITUDE Layer thickness Limfjorden LONGITUDE Paleolatitude Paleolongitude Sampling by hand Dataset 2007 ftpangaea https://doi.org/10.1594/PANGAEA.670359 https://doi.org/10.1007/s00531-006-0085-7 2023-01-20T08:42:31Z 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. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(47.700000,56.900000,13.000000,-13.400000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Area/locality Denmark Jutland Fur_island HAND Isopach area square root LATITUDE Layer thickness Limfjorden LONGITUDE Paleolatitude Paleolongitude Sampling by hand |
spellingShingle |
Area/locality Denmark Jutland Fur_island HAND Isopach area square root LATITUDE Layer thickness Limfjorden LONGITUDE Paleolatitude Paleolongitude Sampling by hand Egger, Hans Brückl, Ewald Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) |
topic_facet |
Area/locality Denmark Jutland Fur_island HAND Isopach area square root LATITUDE Layer thickness Limfjorden LONGITUDE Paleolatitude Paleolongitude Sampling by hand |
description |
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 |
author |
Egger, Hans Brückl, Ewald |
author_facet |
Egger, Hans Brückl, Ewald |
author_sort |
Egger, Hans |
title |
Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) |
title_short |
Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) |
title_full |
Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) |
title_fullStr |
Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) |
title_full_unstemmed |
Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1) |
title_sort |
present day and paleo-geographic coordinates, thicknesses and isopach area of the early eocene +19 ash layer (table 1) |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.670359 https://doi.org/10.1594/PANGAEA.670359 |
op_coverage |
MEDIAN LATITUDE: 8.473333 * MEDIAN LONGITUDE: 54.806667 * SOUTH-BOUND LATITUDE: -13.400000 * WEST-BOUND LONGITUDE: 47.700000 * NORTH-BOUND LATITUDE: 13.000000 * EAST-BOUND LONGITUDE: 56.900000 |
long_lat |
ENVELOPE(47.700000,56.900000,13.000000,-13.400000) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Egger, Hans; Brückl, Ewald (2006): Gigantic volcanic eruptions and climatic change in the early Eocene. International Journal of Earth Sciences, 95, 1065-1070, https://doi.org/10.1007/s00531-006-0085-7 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.670359 https://doi.org/10.1594/PANGAEA.670359 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.670359 https://doi.org/10.1007/s00531-006-0085-7 |
_version_ |
1766132369681547264 |