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Palynology of Aptian and upper Albian (Lower Cretaceous) amber-bearing outcrops of the southern margin of the Basque-Cantabrian basin (northern Spain)

机译:阿巴斯人和巴斯克-坎塔布连盆地(西班牙北部)南部边缘的上琥珀色(下白垩统)琥珀露头的孢粉学

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The Lower Cretaceous deposits of the southern margin of the Basque-Cantabrian basin (northern Spain) are characterised by continental deposits interbedded with amber-bearing marine-influenced facies. These facies crop out in various localities and have yielded well-preserved palynological assemblages. The palynoflora is dominated by gymnosperm pollen grains, and shows relatively diversified spore content but scarce dinoflagellate cysts. The palynofloral evidence and regional geological setting indicate that the studied successions are dated as Aptian (Montoria-La Mina outcrop) and late Albian (Periacerrada 1 and 2 and Salinillas de Buradon outcrops, and the Pancorbo site). Angiosperm pollen does not constitute a significant part of the Aptian assemblages but becomes diversified and numerically abundant in those dated as late Albian. Although broadly similar to contemporaneous palynofloras from eastern Spain, the Aptian assemblages of Montoria-La Mina do not yield tricolpate angiosperm pollen. Conversely, the inferred late Albian assemblages show a high content in polyaperturate angiosperm pollen grains, as occurs in other localities in Portugal, Western Europe and North America. The studied palynoflora shows significant differences from published assemblages located further north, in western France and Canada. (C) 2014 Elsevier Ltd. All rights reserved.
机译:巴斯克-坎塔布连盆地(西班牙北部)南部边缘的下白垩统沉积物以陆相沉积物与含琥珀色的海相相交错为特征。这些相遍布各地,并产生了保存完好的孢粉组合。 ly科植物的裸子植物花粉粒占主导地位,孢子含量相对分散,但鞭毛囊肿稀少。古植物证据和区域地质背景表明,研究的演替年代为Aptian(Montoria-La Mina露头)和Albian晚期(Periacerrada 1和2和Salinillas de Buradon露头,以及Pancorbo遗址)。被子植物的花粉并不构成Aptian组合的重要组成部分,但是在早于Albian的那些中被多样化和数量丰富。尽管与西班牙东部的同时期的古植物广泛相似,Montoria-La Mina的Aptian组合不会产生三足类被子植物花粉。相反,如在葡萄牙,西欧和北美的其他地区所见,推断的晚期阿尔比亚组合在多孔被子植物花粉粒中含量较高。所研究的pa科植物与法国北部和法国北部更远的已发表种群之间存在显着差异。 (C)2014 Elsevier Ltd.保留所有权利。

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