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A review of the chronostratigraphical ages of Middle Triassic to Late Jurassic dinoflagellate cyst biozones of the North West Shelf of Australia

机译:澳大利亚西北陆架中三叠世至晚侏罗世甲藻囊肿生物区年代地层年龄综述

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摘要

The chronostratigraphical ages of the 20 dinoflagellate cyst zones and one dinoflagellate cyst assemblage for the Middle Triassic (Ladinian) to the Jurassic–Cretaceous transition of the North West Shelf of Australia are comprehensively reviewed. Evidence from macro- and micropalaeontology, palynology and strontium isotopes made available after the establishment of these biozones in the 1980s has been used to reassess the ages of this important zonal scheme and to calibrate it to the international stratigraphical stages. The Shublikodinium Superzone is renamed herein as the Rhaetogonyaulax Superzone, and based on conodont evidence is determined to span the Ladinian to Early Sinemurian. This is significantly shorter in duration than was originally envisaged (Late Anisian to Late Pliensbachian). The Luehndea Assemblage is a low diversity dinoflagellate cyst association which marks a eustatic rise; it is subdivided into two subzones. It is of latest Pliensbachian to Early Toarcian age, based largely on palynological evidence. The Bajocian to earliest Oxfordian Pareodinia ceratophora Superzone represents the inception of a continuous Mesozoic–Cenozoic dinoflagellate cyst record in Australia. It comprises seven zones, which are considered to be slightly older than originally interpreted. The overlying Pyxidiella Superzone is characterised by diverse dinoflagellate cyst associations. It is Early Oxfordian to Kimmeridgian in age, and comprises three zones. The bases of the Wanaea spectabilis and Wanaea clathrata zones are reinterpreted as being slightly older than originally proposed. The superjacent Fromea cylindrica Superzone is Tithonian to earliest Valanginian and modified ages are indicated for four of the nine zones. This unit is dominated by endemic dinoflagellate cysts, reflecting a global trend towards provincialism at this time due to a regressive eustatic regime.udud
机译:对澳大利亚西北陆架中三叠纪(拉丁尼亚)至侏罗纪-白垩纪过渡的20个鞭毛囊肿区和一个鞭毛囊肿组合的年代地层年龄进行了全面回顾。这些生物区在1980年代建立之后,从宏观和微观古生物学,孢粉学和锶同位素获得的证据已被用于重新评估这一重要地带方案的年龄,并将其校准到国际地层学阶段。 Shublikodinium超级区在此重命名为Rhaetogonyaulax超级区,并根据牙形体证据确定横跨Ladinian到Early Sinemurian。持续时间明显短于最初设想的时间(晚期阿尼西亚至晚期普林斯巴赫式)。 Luehndea组合是低多样性的鞭毛囊肿协会,标志着欣喜若狂。它分为两个分区。它主要是在孢粉学证据的基础上,是普林斯巴赫时代到早期的Toarcian时代。巴约西亚人到最早的牛津帕雷迪亚角藻超级区代表了澳大利亚连续的中,新生代鞭毛虫囊肿记录的开始。它包括七个区域,被认为比最初解释的区域稍早。上层的毕生球菌超级区的特征是多种鞭毛藻囊肿协会。它的年龄是早期的牛津到基米吉丁,包括三个区域。 Wanaea spectabilis和Wanaea clathrata带的基地被重新解释为比最初提出的要稍旧。毗邻的Fromea cylindrica Superzone是Tithonian到最早的Valanginian,在这9个区域中有4个的年龄已被修改。该单位以地方性鞭毛囊肿为主导,反映了由于回归性的欣欣向荣政权,这时全球趋向省级主义的趋势。 ud ud

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