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dc.contributor.author
Sial, A. N.
dc.contributor.author
Chen, Jiubin
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Lacerda, L. D.
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Frei, R.
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Tewari, V. C.
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Pandit, M. K.
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Gaucher, C.
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Ferreira, V. P.
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Cirilli, S.
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Peralta, Silvio Heriberto
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Korte, C.
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Barbosa, J. A.
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Pereira, N. S.
dc.date.available
2018-09-28T15:01:06Z
dc.date.issued
2016-11
dc.identifier.citation
Sial, A. N.; Chen, Jiubin; Lacerda, L. D.; Frei, R.; Tewari, V. C.; et al.; Mercury enrichment and Hg isotopes in Cretaceous-Paleogene boundary successions: Links to volcanism and palaeoenvironmental impacts; Academic Press Ltd - Elsevier Science Ltd; Cretaceous Research; 66; 11-2016; 60-81
dc.identifier.issn
0195-6671
dc.identifier.uri
http://hdl.handle.net/11336/61198
dc.description.abstract
We investigate the use of Hg as a proxy for volcanism by studying four distal and two proximal sections in relation to the Deccan volcanic center, straddling the Cretaceous-Paleogene (KPg) boundary at (a) Højerup (Denmark), Bottaccione and Padriciano (Italy), (b) Meghalaya and Jhilmili (India), and (c) Bajada del Jagüel (Argentina). Hg sequestration by organic matter results in constant Hg/TOC ratio and linear correlation between Hg content of the sediments and total organic carbon (TOC).Elevated Hg concentrations that deviate from this linear relationship represent most likely true Hg anomalies and these notable Hg/TOC spikes (all TOC <1%) are found in the Meghalaya, Bottaccione and Højerup sections within the CF2 planktic foraminiferal biozone (spike I), at the KPg boundary (spike II), and within the P1a planktic foraminiferal subzone (spike III). Spike III occurs also in the Jhilmili section. No clear correlation between Hg/TOC and Al2O3 exists in any of the studied sections. The Hg anomalies probably result from strong volcanic episodes of the Deccan phase-2 (started 250 kyr before the KPg boundary and lasted for 750 kyr) that exhaled sulfuric aerosols, carbon dioxide and other toxic agents which reached a critical threshold, represented in true Hg enrichments in the paleoenvironments. The possibility that Hg enrichments resulted from anoxia scavenging on the seafloor and penetration downward into sediments is not supported in the stratigraphic record of Mo/Al ratios redox proxy.Hg isotopes were analyzed in samples from all KPg boundary sections in this study and from Bidart, France, the latter for comparison. Hg isotopes yielded δ202Hg values ranging from -1 to -2‰ and δ201Hg signatures from 0 to 0.05‰ (spike II in Højerup, Bottaccione and Meghalaya KPg boundary layers) consistent with volcanic emission of Hg (0 to -2‰). The δ202Hg in spike I in Meghalaya and Padriciano and spike III in Jhilmili is consistent with volcanic emission of Hg. Two samples from Bajada del Jagüel and four from Bidart, however, display isotope signals compatible with volcanic emission/chondrite Hg. The results of three other samples are characteristic for reworked sediment, soil and/or peat. Most of the data show small positive Δ201Hg, in favor of long-term atmospheric transport prior to deposition, supporting a volcanic origin for the Hg. The present study broadens, therefore, the potential use of Hg as stratigraphic marker and, moreover, confirms that in the critical KPg transition, Hg was enriched in paleoenvironments at three distinct stages during the Deccan phase-2.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Academic Press Ltd - Elsevier Science Ltd
dc.rights
info:eu-repo/semantics/openAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.subject
Chemostratigraphy
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Cretaceous-Paleogene Boundary
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Hg Isotopes
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Molybdenum
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Total Organic Carbon
dc.subject.classification
Geoquímica y Geofísica
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Ciencias de la Tierra y relacionadas con el Medio Ambiente
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CIENCIAS NATURALES Y EXACTAS
dc.title
Mercury enrichment and Hg isotopes in Cretaceous-Paleogene boundary successions: Links to volcanism and palaeoenvironmental impacts
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2018-09-27T20:15:39Z
dc.journal.volume
66
dc.journal.pagination
60-81
dc.journal.pais
Estados Unidos
dc.description.fil
Fil: Sial, A. N.. Universidade Federal de Pernambuco; Brasil
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Fil: Chen, Jiubin. Chinese Academy of Sciences; República de China
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Fil: Lacerda, L. D.. Universidade Federal do Ceará; Brasil
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Fil: Frei, R.. Universidad de Copenhagen; Dinamarca
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Fil: Tewari, V. C.. Sikkim University; India
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Fil: Pandit, M. K.. Rajasthan University; India
dc.description.fil
Fil: Gaucher, C.. Universidad de la República. Facultad de Ciencias; Uruguay
dc.description.fil
Fil: Ferreira, V. P.. Universidade Federal de Pernambuco; Brasil
dc.description.fil
Fil: Cirilli, S.. Università di Perugia; Italia
dc.description.fil
Fil: Peralta, Silvio Heriberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan. Centro de Investigaciones de la Geosfera y Biosfera. Universidad Nacional de San Juan. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones de la Geosfera y Biosfera; Argentina
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Fil: Korte, C.. Universidad de Copenhagen; Dinamarca
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Fil: Barbosa, J. A.. Universidade Federal de Pernambuco; Brasil
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Fil: Pereira, N. S.. Universidade do Estado da Bahia; Brasil
dc.journal.title
Cretaceous Research
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.cretres.2016.05.006
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0195667116300969
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