阿尔巴尼亚-塞萨利亚盆地下中新世钙质纳米化石与古环境的生物地层学

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Geologica Carpathica Pub Date : 2023-06-27 DOI:10.31577/geolcarp.2023.01
Mădălina-Elena Kallanxhi
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引用次数: 1

摘要

阿尔巴尼亚-塞萨利亚盆地位于莫拉瓦山附近,包括始新世至中新世中期的沉积物,其中含有鲜为人知的钙质纳米化石含量。本研究重点研究了该区下中新世露头沉积物中的钙质纳米化石组合,并与全球纳米化石带/亚带NN2-NN3 / CN1c-CN2进行了对比,并与地中海地区的生物带MNN2b和MNN3a进行了对比。主要和次要指标种(ampliaperta Helicosphaera, mediterranea Helicosphaera, Sphenolithus belemnos, Sphenolithus disbelemnos, Sphenolithus pseudoheteromorphus)支持了研究露头早-中期burdigaria时代。对钙质纳米化石进行了定量分析,并对所有计数样本进行了统计。基于统计分析,通过钙质纳米化石组合及其丰度模式的变化,记录了温度、盐度和富营养化等古环境参数的短期波动。沉积古环境反映了盆地水深的变化,受冷上升流、陆源营养物流入的影响,古环境扰动在短时间间隔内增加
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Biostratigraphy of calcareous nannofossils and palaeoenvironments in the Lower Miocene of the Albanian–Thessalian Basin (Albania)
: The Albanian–Thessalian Basin, which is located in the vicinity of Mount Morava, includes Eocene to Middle Miocene sediments with a poorly-known, calcareous nannofossil content. This study is focused on the investigation of calcareous nannofossil assemblages from the Lower Miocene sediments outcropping in the area, resulting in the correlation to the global nannofossils zones/subzones NN2–NN3/CN1c–CN2, as well as to the zonation from the Mediterranean area, where the MNN2b and MNN3a biozones have been identified. An early-middle Burdigalian age for the studied outcrops is supported by primary and secondary index species ( Helicosphaera ampliaperta , Helicosphaera mediterranea , Sphenolithus belemnos , Sphenolithus disbelemnos , Sphenolithus pseudoheteromorphus ). Quantitative analyses were performed on calcareous nannofossils and statistics were applied to all of the counted samples. Based on the statistical analysis, short-time fluctuations in palaeoenvironmental parameters, such as temperature, salinity and eutrophic regime, are documented through the changes in the calcareous nannofossil assemblages and their abundance patterns. The depositional palaeoenvironment indicates changes in basin water depth, with influence of cold upwelling currents, terrigenous nutrient influx, and increased palaeoenvironmental perturbations over short time intervals
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来源期刊
Geologica Carpathica
Geologica Carpathica 地学-地球科学综合
CiteScore
2.40
自引率
23.10%
发文量
26
审稿时长
>12 weeks
期刊介绍: GEOLOGICA CARPATHICA covers a wide spectrum of geological disciplines including geodynamics, tectonics and structural geology, volcanology, stratigraphy, geochronology and isotopic geology, karstology, geochemistry, mineralogy, petrology, lithology and sedimentology, paleogeography, paleoecology, paleobiology and paleontology, paleomagnetism, magnetostratigraphy and other branches of applied geophysics, economic and environmental geology, experimental and theoretical geoscientific studies. Geologica Carpathica , with its 60 year old tradition, presents high-quality research papers devoted to all aspects not only of the Alpine-Carpathian-Balkanian geoscience but also with adjacent regions originated from the Mediterranean Tethys and its continental foreland. Geologica Carpathica is an Official Journal of the Carpathian-Balkan Geological Association.
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