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  • Kenya tuffs Rev2 (Claessens et al., 2016)

    Rights statement: This is the author’s version of a work that was accepted for publication in Global and Planetary Change. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Global and Planetary Change, 145, 2016 DOI: 10.1016/gloplacha.2016.08.006

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Large scale pantelleritic ash flow eruptions during the Late Miocene in central Kenya and evidence for significant environmental impact

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Large scale pantelleritic ash flow eruptions during the Late Miocene in central Kenya and evidence for significant environmental impact. / Claessens, L. ; Veldkamp, A.; Schoorl, J. R. ; Wijbrans, J. R.; van Gorp, W.; MacDonald, Raymond.

In: Global and Planetary Change, Vol. 145, 10.2016, p. 30-41.

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Claessens, L. ; Veldkamp, A. ; Schoorl, J. R. ; Wijbrans, J. R. ; van Gorp, W. ; MacDonald, Raymond. / Large scale pantelleritic ash flow eruptions during the Late Miocene in central Kenya and evidence for significant environmental impact. In: Global and Planetary Change. 2016 ; Vol. 145. pp. 30-41.

Bibtex

@article{0ede1386f8bc4bd69bf3e79ab2b418c4,
title = "Large scale pantelleritic ash flow eruptions during the Late Miocene in central Kenya and evidence for significant environmental impact",
abstract = "In the area south-east of Mount Kenya, four previously unrecorded peralkaline rhyolitic (pantelleritic) ash flow tuffs have been located. These predominantly greyish welded and non-welded tuffs form up to 12 m thick units, which are sometimes characterized by a basal vitrophyre. The four flow units yielded 40Ar/39Ar ages ranging from 6.36 to 8.13 Ma, indicating a period of ~ 1.8 Ma of pantelleritic volcanic activity during the Late Miocene in central Kenya. Tentative compositional and age correlations with other known tuff deposits suggest that the pantelleritic tuffs originally covered 40,000 km2 in central Kenya, extending much further than earlier recorded Pliocene tuffs. This newly identified magmatic phase occurred between the phonolitic flood eruptions (16–8 Ma) and the Pliocene tuff eruptions (6–4 Ma). The occurrence of multiple ash flow tuff deposits up to 150 km away from the inferred eruptive center(s) in the central sector of the Kenya Rift, indicates multi-cyclic peralkaline supereruptions during the Late Miocene. By analogy with more recent pantelleritic eruptions, the tuffs are thought to have been sulfur-rich; during eruption, they formed stratospheric aerosols, with significant environmental impact. The timing of the eruptions coincides with the shift towards more savannah-dominated environments in East Africa.",
keywords = "Tuff, Ash flow, Ignimbrite, Vitrophyre, Peralkaline rhyolites, 40Ar/39Ar geochronology",
author = "L. Claessens and A. Veldkamp and Schoorl, {J. R.} and Wijbrans, {J. R.} and {van Gorp}, W. and Raymond MacDonald",
note = "This is the author{\textquoteright}s version of a work that was accepted for publication in Global and Planetary Change. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Global and Planetary Change, 145, 2016 DOI: 10.1016/gloplacha.2016.08.006",
year = "2016",
month = oct,
doi = "10.1016/j.gloplacha.2016.08.006",
language = "English",
volume = "145",
pages = "30--41",
journal = "Global and Planetary Change",
issn = "0921-8181",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Large scale pantelleritic ash flow eruptions during the Late Miocene in central Kenya and evidence for significant environmental impact

AU - Claessens, L.

AU - Veldkamp, A.

AU - Schoorl, J. R.

AU - Wijbrans, J. R.

AU - van Gorp, W.

AU - MacDonald, Raymond

N1 - This is the author’s version of a work that was accepted for publication in Global and Planetary Change. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Global and Planetary Change, 145, 2016 DOI: 10.1016/gloplacha.2016.08.006

PY - 2016/10

Y1 - 2016/10

N2 - In the area south-east of Mount Kenya, four previously unrecorded peralkaline rhyolitic (pantelleritic) ash flow tuffs have been located. These predominantly greyish welded and non-welded tuffs form up to 12 m thick units, which are sometimes characterized by a basal vitrophyre. The four flow units yielded 40Ar/39Ar ages ranging from 6.36 to 8.13 Ma, indicating a period of ~ 1.8 Ma of pantelleritic volcanic activity during the Late Miocene in central Kenya. Tentative compositional and age correlations with other known tuff deposits suggest that the pantelleritic tuffs originally covered 40,000 km2 in central Kenya, extending much further than earlier recorded Pliocene tuffs. This newly identified magmatic phase occurred between the phonolitic flood eruptions (16–8 Ma) and the Pliocene tuff eruptions (6–4 Ma). The occurrence of multiple ash flow tuff deposits up to 150 km away from the inferred eruptive center(s) in the central sector of the Kenya Rift, indicates multi-cyclic peralkaline supereruptions during the Late Miocene. By analogy with more recent pantelleritic eruptions, the tuffs are thought to have been sulfur-rich; during eruption, they formed stratospheric aerosols, with significant environmental impact. The timing of the eruptions coincides with the shift towards more savannah-dominated environments in East Africa.

AB - In the area south-east of Mount Kenya, four previously unrecorded peralkaline rhyolitic (pantelleritic) ash flow tuffs have been located. These predominantly greyish welded and non-welded tuffs form up to 12 m thick units, which are sometimes characterized by a basal vitrophyre. The four flow units yielded 40Ar/39Ar ages ranging from 6.36 to 8.13 Ma, indicating a period of ~ 1.8 Ma of pantelleritic volcanic activity during the Late Miocene in central Kenya. Tentative compositional and age correlations with other known tuff deposits suggest that the pantelleritic tuffs originally covered 40,000 km2 in central Kenya, extending much further than earlier recorded Pliocene tuffs. This newly identified magmatic phase occurred between the phonolitic flood eruptions (16–8 Ma) and the Pliocene tuff eruptions (6–4 Ma). The occurrence of multiple ash flow tuff deposits up to 150 km away from the inferred eruptive center(s) in the central sector of the Kenya Rift, indicates multi-cyclic peralkaline supereruptions during the Late Miocene. By analogy with more recent pantelleritic eruptions, the tuffs are thought to have been sulfur-rich; during eruption, they formed stratospheric aerosols, with significant environmental impact. The timing of the eruptions coincides with the shift towards more savannah-dominated environments in East Africa.

KW - Tuff

KW - Ash flow

KW - Ignimbrite

KW - Vitrophyre

KW - Peralkaline rhyolites

KW - 40Ar/39Ar geochronology

U2 - 10.1016/j.gloplacha.2016.08.006

DO - 10.1016/j.gloplacha.2016.08.006

M3 - Journal article

VL - 145

SP - 30

EP - 41

JO - Global and Planetary Change

JF - Global and Planetary Change

SN - 0921-8181

ER -