Análise isotópica de oxigênio e carbono em microfósseis da Formação Romualdo, cretáceo inferior, bacia do Araripe, Pernambuco, nordeste do Brasil

Rilda Verônica Cardoso de Araripe, David Holanda de Oliveira, Maria Emília Travassos Rios Tomé, R. M. Mello, A. F. Barreto, A. N. Sial
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引用次数: 2

Abstract

This work presents the analysis of C and O isotope values behavior in the carapace of ostracodes and foraminifera from the Romualdo Formation, Araripe Basin – PE. The analized samples were collected in three outcrops (Arrojado, Canastra and Cedro) located in the cities of Exu and Araripina. The de δ 18 O values ranged from -10.1‰ to -10.2‰ VPDB and the δ 13 C values ranged between -12,6‰ to +2.7‰ VPDB. The results for oxygen data indicate high temperature of waters and the deposition of marine limestones in all outcrops. For the carbon isotopic data in the Arrojado and Canastra outcrops, the values indicate an anoxic environment with high content of organic matter. In Cedro outcrop, a positive variation occurs indicating an increase in primary production, also associated to an anoxic event, and the positive values are interpreted as a transgressive pulse. These results indicate that Cedro outcrop, located in the middlesouth portion of the basin, has environmental characteristics with greater marine influence than in the Arrojado and Canastra outcrops, located in the southwest portion.
巴西东北部伯南布哥Ara熟盆地下白垩统Romualdo组微体化石中氧和碳的同位素分析
这项工作分析了Ara熟盆地Romualdo组介形虫和有孔虫外壳中的C和O同位素值行为。分析样本采集于Exu和Araripina市的三个露头(Arrojado、Canastra和Cedro)。deδ18O值范围为-10.1‰至-10.2‰VPDB,δ13C值范围为-12.6‰至+2.7‰VPDB。氧气数据的结果表明,海水温度很高,所有露头都有海洋石灰岩沉积。对于Arrojado和Canastra露头的碳同位素数据,这些值表明存在高有机质含量的缺氧环境。在Cedro露头中,出现正变化,表明初级产量增加,这也与缺氧事件有关,正值被解释为海侵脉冲。这些结果表明,位于盆地中南部的Cedro露头具有比位于西南部的Arrojado和Canastra露头更大的海洋影响的环境特征。
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