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  1. 原著論文

Unraveling the record of a tropical continental Cretaceous-Paleogene boundary in northern Colombia, South America

https://repo.qst.go.jp/records/84911
https://repo.qst.go.jp/records/84911
e3cf1135-6edc-464b-ac3b-a350a7d43570
Item type 学術雑誌論文 / Journal Article(1)
公開日 2022-02-02
タイトル
タイトル Unraveling the record of a tropical continental Cretaceous-Paleogene boundary in northern Colombia, South America
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
アクセス権
アクセス権 metadata only access
アクセス権URI http://purl.org/coar/access_right/c_14cb
著者 de laParra, Felipe

× de laParra, Felipe

WEKO 1040787

de laParra, Felipe

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Jaramillo, Carlos

× Jaramillo, Carlos

WEKO 1040788

Jaramillo, Carlos

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Kaskes, Pim

× Kaskes, Pim

WEKO 1040789

Kaskes, Pim

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Goderis, Steven

× Goderis, Steven

WEKO 1040790

Goderis, Steven

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Claeys, Philippe

× Claeys, Philippe

WEKO 1040791

Claeys, Philippe

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Víctor, Villasante-Marcos

× Víctor, Villasante-Marcos

WEKO 1040792

Víctor, Villasante-Marcos

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Bayona, German

× Bayona, German

WEKO 1040793

Bayona, German

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Yuuichi, Hatsukawa

× Yuuichi, Hatsukawa

WEKO 1040794

Yuuichi, Hatsukawa

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Yuuichi, Hatsukawa

× Yuuichi, Hatsukawa

WEKO 1040795

en Yuuichi, Hatsukawa

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抄録
内容記述タイプ Abstract
内容記述 The Cretaceous-Paleogene (K-Pg) boundary event, triggered by the Chicxulub asteroid impact in Mexico ∼66 Myr ago, is recognized as one of the major environmental crises in Earth's history. Its effects on the evolution of tropical vegetation were drastic, giving rise to the closed-canopy tropical rainforest. Despite of its importance, the actual K-Pg boundary event layer has not yet been identified in terrestrial sections within tropical latitudes. Here, we study a sediment core (Diablito-1) from northern Colombia and described its lithofacies, palynostratigraphic content, magnetic susceptibility and geochemical composition, including the concentration of key elements linked to a meteoritic contribution such as iridium. We found an 8.2 cm-thick (0.27 inches) interval with gravel-size calcareous intraclasts, broken skeletal fragments and siliceous spherules that were transported during a short-duration high-energy event into the coastal plain. Very fine-to medium-grained spherules, concentrated in several layers of the flow structure, could be interpreted as derived from the K-Pg impact event. This thin intraclastic packstone interval lies within the extinction level of the palynomorph Echimonocolpites franciscoi, an important biostratigraphic event associated with the K-Pg boundary in Colombia. In addition, this layer is associated with both a small iridium anomaly and high concentration of several other major and trace elements that are occurring above a low Magnetic Susceptibility (MS) interval and within the initial phase of a high MS interval. These lines of evidence support the position of the K-Pg event layer within the thin interval that includes the spherules in the Diablito-1 core.
書誌情報 Journal of South American Earth Sciences

巻 114, p. 103717, 発行日 2022-02
出版者
出版者 Elsevier
ISSN
収録物識別子タイプ ISSN
収録物識別子 0895-9811
DOI
識別子タイプ DOI
関連識別子 10.1016/j.jsames.2022.103717
関連サイト
識別子タイプ URI
関連識別子 https://www.sciencedirect.com/science/article/abs/pii/S0895981122000086
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