globalchange  > 过去全球变化的重建
DOI: 10.1016/j.palaeo.2013.12.031
论文题名:
Late Barremian-early Aptian dark facies of the Subbetic (Betic Cordillera, southern Spain): Calcareous nannofossil quantitative analyses, chemostratigraphy and palaeoceanographic reconstructions
作者: Aguado R.; de Gea G.A.; Castro J.M.; O'Dogherty L.; Quijano M.L.; Naafs B.D.A.; Pancost R.D.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2014
卷: 395
起始页码: 198
结束页码: 221
语种: 英语
英文关键词: Calcareous nannofossils ; Chemostratigraphy ; Latest Barremian-early Aptian ; Palaeoceanography ; Planktonic foraminifera ; Radiolaria
英文摘要: In order to determine the driving mechanism behind the deposition of the Aptian dark facies in the pelagic Subbetic Basin (southern Spain), two latest Barremian-early Aptian complementary sections embracing the Oceanic Anoxic Event 1a, were selected for a multidisciplinary study. Quantitative and statistical analyses of calcareous nannofossil assemblages are complemented with planktonic foraminifera, radiolaria, and geochemical data (C and O isotopes and biomarkers). The results indicate that most of the latest Barremian was characterized by oligotrophic conditions with a low nutricline and neritic influence, which were interrupted by short-lived episodes of mesotrophic surface waters. In contrast, broadly meso-eutrophic surface waters with a high nutricline and a probable development of water stratification are inferred for most of the early Aptian. It is suggested that an increased runoff, as a consequence of a more humid climate in the adjacent continental area, caused this fertilization. Neritic dwellers, such as nannoconids and pentaliths, experienced a drastic decrease in abundance as the result of the combined effects of a biocalcification crisis ('nannoconid crisis') and the deepening of the basin. High productivity and enhanced surface-water stratification favoured low oxygen content in the bottom waters, increasing organic matter preservation. A reduction in surface water fertility and a shift towards generally cooler conditions occurred during the late early Aptian. It is postulated that a cooler and drier climate leads to a reduction in runoff and decreased nutrient flux into the basin. The obtained results suggest that the formation of the Aptian dark facies was mainly controlled by enhanced production of organic matter in the upper water column and not enhanced preservation. © 2013 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69474
Appears in Collections:过去全球变化的重建

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作者单位: Departamento de Geología and CEACTierra, Universidad de Jaén, EPS Linares, E-23700 Linares, Spain; Departamento de Geología and CEACTierra, Universidad de Jaén, Campus Las Lagunillas, E-23071 Jaén, Spain; Departamento de Ciencias de la Tierra, Universidad de Cádiz, CASEM, E-11510 Puerto Real, Spain; Departamento de Química Orgánica e Inorgánica and CEACTierra, Universidad de Jaén, Campus Las Lagunillas, E-23071 Jaén, Spain; Organic Geochemistry Unit, The Cabot Institute, School of Chemistry, University of Bristol, BS8 1TS, United Kingdom

Recommended Citation:
Aguado R.,de Gea G.A.,Castro J.M.,et al. Late Barremian-early Aptian dark facies of the Subbetic (Betic Cordillera, southern Spain): Calcareous nannofossil quantitative analyses, chemostratigraphy and palaeoceanographic reconstructions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2014-01-01,395
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