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The Dan-C2 Hyperthermal Event at Gubbio (Italy): Global Implications, Environmental Effects and Cause(s) (Articolo in rivista)
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- Label
- The Dan-C2 Hyperthermal Event at Gubbio (Italy): Global Implications, Environmental Effects and Cause(s) (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Alternative label
R.Coccioni, F. Frontalini, G.Bancalà, E.Fornaciari, L.Jovane, M.Sprovieri. (2010)
The Dan-C2 Hyperthermal Event at Gubbio (Italy): Global Implications, Environmental Effects and Cause(s)
in Earth and planetary science letters
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- R.Coccioni, F. Frontalini, G.Bancalà, E.Fornaciari, L.Jovane, M.Sprovieri. (literal)
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- Dipartimento di Scienze dell'Uomo, dell'Ambiente e della Natura, Università di Urbino, Urbino, Italy; Dipartimento di Geoscienze, Università di Padova, Padova, Italy; Department of Geology, Western Washington University, Bellingham, USA; Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy; Istituto Ambiente Marino Costiero, Consiglio Nazionale delle Ricerche, Trapani, Italy (literal)
- Titolo
- The Dan-C2 Hyperthermal Event at Gubbio (Italy): Global Implications, Environmental Effects and Cause(s) (literal)
- Abstract
- The Dan-C2 event is an early Danian, transient (~100 kyr) hyperthermal episode centered at ~65.2 Ma,
which records shifts in carbon reservoirs and ocean warming in the northwestern and southeastern sectors
of the Atlantic Ocean. Here we present and discuss high-resolution biochronostratigraphic and magnetic
susceptibility data and geochemical records from the western Tethyan Contessa Highway section (Gubbio,
Italy), which provide the first direct evidence of the Dan-C2 event beyond the Atlantic Ocean and point to the
supra-regional, possibly global, significance thereof. At Contessa Highway, the Dan-C2 event exhibits
stressed ecological responses among calcareous nannoplankton and foraminifera, which highlight marked
environmental perturbation affecting the geobiosphere and resulting in enhanced eutrophication of the sea
surface waters and carbonate dissolution, as well as lowered oxygen content along the water column and at
the sea bottom. As for other early Paleogene hyperthermal events, the cause of the Dan-C2 event might likely
to be found in changes, potentially astronomically paced, in the distribution of carbon within surface
biosphere reservoirs. However, the role played by the concurrent third and last phase of Deccan volcanism
with its huge release of greenhouse gases into the atmosphere would be also taken into account.
In addition, here we provide first evidence of a further short-lived (~38 kyr) hyperthermal event not known
up to now and that we term the \"Lower C29n\" event. (literal)
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