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An isolated carbonate knoll in the Timor Sea (Sahul Shelf, NW Australia): facies zonation and sediment composition

机译:东帝汶的一个孤立的碳酸盐丘陵(澳大利亚西北部萨胡尔架):相带划分和沉积物组成

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摘要

This paper constitutes a first detailed and systematic facies and biota description of an isolated carbonate knoll (Pee Shoal) in the Timor Sea (Sahul Shelf, NW Australia). The steep and flat-topped knoll is characterized by a distinct facies zonation comprising (A) soft sediments with scattered debris and scarce sponges, hydrozoans and crinoids (320–210 m water depth), (B) hardground outcrops (step-like banks, vertical cliffs) that are mainly colonized by octocorals and sponges (210–75 m), and (C) the summit region (75–21 m) where the slopes merge gently into the flat-topped summit that is densely colonized by massive and encrusting zooxanthellate corals and the octocoral Heliopora coerulea. In contrast, the sediments recovered from the summit are dominated by the green alga Halimeda, subordinate components are corals, benthic foraminifers, mollusks, and coralline red algae. Thus, the sediments are classified as chlorozoan grain assemblage. However, non-skeletal grains (fecal pellets, ooids) are almost completely absent. This discrepancy between the living biota and the sediment composition could reflect a disruption by the severe tropical cyclone Ingrid that hit the northern Australian shelf in March 2005, just before the sampling for this study took place (September 2005).
机译:本文构成了帝汶海(澳大利亚西北部Sahul Shelf)一个孤立的碳酸盐丘(小便浅滩)的第一个详细的系统化相和生物群描述。陡峭而平顶的丘陵具有明显的相带特征,包括(A)具有分散的碎屑和稀少的海绵,水生动物和海百合(水深320-210 m)的软沉积物,(B)硬地露头(阶梯状河岸,垂直悬崖)主要由八角形和海绵(210–75 m)定居;(C)山顶区域(75–21 m),斜坡逐渐融合成平顶山顶,并被大量块状硬壳殖民虫黄藻珊瑚和八叶Heliopora coerulea。相比之下,从山顶回收的沉积物主要由绿藻Halimeda占据,下属成分是珊瑚,底栖有孔虫,软体动物和珊瑚红藻。因此,沉积物被归类为绿藻类颗粒组合。但是,几乎完全没有非骨骼的谷物(粪便颗粒,卵石)。活生物群和沉积物成分之间的差异可能反映了严重的热带气旋英格丽德(Ingrid)的破坏,该气旋于2005年3月袭击了澳大利亚北部的架子,就在该研究取样之前(2005年9月)。

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