1998
DOI: 10.1038/32871
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Low-sea-level emplacement of a very large Late Pleistocene ‘megaturbidite’ in the western Mediterranean Sea

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Cited by 163 publications
(112 citation statements)
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References 24 publications
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“…Canyon and on the Porcupine slope (Øvrebø et al, 2006;Voigt et al, 2013). We propose that this process may pre-condition the down-current slope to failure via increased sedimentation of fine material and possible undercutting of the deposited material by the adjacent current stream, in a manner similar to that suggested for the Rockall Bank Mass et al, 1995; Øvrebø et al, 2006); changes sediment provenance (Rothwell et al, 1998;Hemming, 2004); porosity and density variation (Goff et al, 2004);…”
Section: Accepted Manuscriptmentioning
confidence: 68%
“…Canyon and on the Porcupine slope (Øvrebø et al, 2006;Voigt et al, 2013). We propose that this process may pre-condition the down-current slope to failure via increased sedimentation of fine material and possible undercutting of the deposited material by the adjacent current stream, in a manner similar to that suggested for the Rockall Bank Mass et al, 1995; Øvrebø et al, 2006); changes sediment provenance (Rothwell et al, 1998;Hemming, 2004); porosity and density variation (Goff et al, 2004);…”
Section: Accepted Manuscriptmentioning
confidence: 68%
“…The global peak energy is 8.4 × 10 14 J (0.2 Megatons). When compared with the gap of gravitational potential energy in the prescribed motion (3.4 × 10 16 J, from Eq. 7), the conversion factor (referred to the peak) is 2.8%, within the range of usual values found in literature (e.g.…”
Section: Model Resultsmentioning
confidence: 99%
“…Paull et al (1996), Rothwell et al (1998), and Nisbet & Piper (1998) document large-scale submarine slides and associated isotopic excursions toward 13 Cdepleted values in late Quaternary sediments, which they interpret as catastrophic methane release after slope failure. These slumps may have been triggered by lowering of hydrostatic pressure due to sea-level low-stand during glacial maxima, resulting in destabilisation of methane clathrates.…”
Section: Highly Depleted 8 I3 C Values: Ancient Clathratesmentioning
confidence: 87%
“…Following this scenario, several "clathrate-burps" could have provided the volume of isotopically depleted methane carbon to the atmosphere (>1 X 10 18 g carbon; Dickens et al 1995) to produce a shift in die global isotopic signature. This mechanism has been proposed for the late Pleistocene (20 000 yr ago) after emplacement of a megaturbidite and associated methane release (Rothwell et al 1998).…”
Section: Highly Depleted 8 I3 C Values: Ancient Clathratesmentioning
confidence: 98%