Rare earth elements (REE) and other trace element concentrations in proximal Chicxulub ejecta deposits from northern Belize – support for a single-impact scenario
(2007) In Meteoritics and Planetary Science 42(11). p.1859-2031- Abstract
- Four exposures of Chicxulub impact ejecta along the Mexico-Belize border have been sampled and analyzed for major and trace element abundances.
The ejecta deposits consist of a lower spheroid bed, containing clay and dolomite spheroids, and an upper diamictite bed with boulders and clasts of limestone and dolomite. The matrix of both beds is composed of clay and micritic dolomite. The rare earth element (REE) compositions in the matrix of both units show strong similarities in concentrations and pattern. Furthermore, the Zr/TiO2 scatter plot shows a linear correlation indicating one source. These results indicate that the basal spheroid bed has the same source and was generated during the same event as the overlying... (More) - Four exposures of Chicxulub impact ejecta along the Mexico-Belize border have been sampled and analyzed for major and trace element abundances.
The ejecta deposits consist of a lower spheroid bed, containing clay and dolomite spheroids, and an upper diamictite bed with boulders and clasts of limestone and dolomite. The matrix of both beds is composed of clay and micritic dolomite. The rare earth element (REE) compositions in the matrix of both units show strong similarities in concentrations and pattern. Furthermore, the Zr/TiO2 scatter plot shows a linear correlation indicating one source. These results indicate that the basal spheroid bed has the same source and was generated during the same event as the overlying diamictite bed, which lends support to a single-impact scenario for the Albion Formation ejecta deposits.
The elevated concentrations of non-meteoritic elements such as Sb, As, U, and Zn in the matrix of the lower spheroid bed are regarded to have been derived from the sedimentary target rocks at the Chicxulub impact site. The positive Eu and Ce anomalies in clay concretion and in the matrix of the lower part of the spheroid bed in Albion Island quarry is probably related to processes involved in the impact, such as high temperature and oxidizing conditions.
Analogous trace element anomalies have been reported from the distal Cretaceous-Paleogene (K/T) boundary clay layer at different sites. Thus, the trace element signals, reported herein, are regarded to support a genetic link between the Chicxulub impact, the ejecta deposits along the Mexico-Belize border, and the global K/T boundary layer. (Less)
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https://lup.lub.lu.se/record/939610
- author
- Wigforss-Lange, Jane LU ; Vajda, Vivi LU and Ocampo, Adriana
- organization
- publishing date
- 2007
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Meteoritics and Planetary Science
- volume
- 42
- issue
- 11
- pages
- 1859 - 2031
- publisher
- Wiley-Blackwell
- external identifiers
-
- scopus:41549128560
- ISSN
- 1086-9379
- language
- English
- LU publication?
- yes
- id
- cb59e2da-260f-4c56-a55f-a36ab21321bb (old id 939610)
- date added to LUP
- 2016-04-01 15:18:19
- date last changed
- 2022-01-28 04:43:09
@article{cb59e2da-260f-4c56-a55f-a36ab21321bb, abstract = {{Four exposures of Chicxulub impact ejecta along the Mexico-Belize border have been sampled and analyzed for major and trace element abundances.<br/><br> <br/><br> The ejecta deposits consist of a lower spheroid bed, containing clay and dolomite spheroids, and an upper diamictite bed with boulders and clasts of limestone and dolomite. The matrix of both beds is composed of clay and micritic dolomite. The rare earth element (REE) compositions in the matrix of both units show strong similarities in concentrations and pattern. Furthermore, the Zr/TiO2 scatter plot shows a linear correlation indicating one source. These results indicate that the basal spheroid bed has the same source and was generated during the same event as the overlying diamictite bed, which lends support to a single-impact scenario for the Albion Formation ejecta deposits.<br/><br> <br/><br> The elevated concentrations of non-meteoritic elements such as Sb, As, U, and Zn in the matrix of the lower spheroid bed are regarded to have been derived from the sedimentary target rocks at the Chicxulub impact site. The positive Eu and Ce anomalies in clay concretion and in the matrix of the lower part of the spheroid bed in Albion Island quarry is probably related to processes involved in the impact, such as high temperature and oxidizing conditions.<br/><br> <br/><br> Analogous trace element anomalies have been reported from the distal Cretaceous-Paleogene (K/T) boundary clay layer at different sites. Thus, the trace element signals, reported herein, are regarded to support a genetic link between the Chicxulub impact, the ejecta deposits along the Mexico-Belize border, and the global K/T boundary layer.}}, author = {{Wigforss-Lange, Jane and Vajda, Vivi and Ocampo, Adriana}}, issn = {{1086-9379}}, language = {{eng}}, number = {{11}}, pages = {{1859--2031}}, publisher = {{Wiley-Blackwell}}, series = {{Meteoritics and Planetary Science}}, title = {{Rare earth elements (REE) and other trace element concentrations in proximal Chicxulub ejecta deposits from northern Belize – support for a single-impact scenario}}, volume = {{42}}, year = {{2007}}, }