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Bromalites from the Cambrian (Series 2 and 3) of North Greenland

机译:北格陵兰的寒武纪(系列2和3)中的溴化岩

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摘要

Six assemblages of phosphatized bromalites from the Cambrian (Series 2 and 3) of North Greenland provide added insight into community structure in fossil assemblages otherwise dominated by microscopic skeletonized organisms. The bromalites, picked from acetic acid residues, display a wide range of morphologies, including pellets, segmented rods, wrinkled, smooth and segmented convoluted strings. Most are interpreted as extruded faecal material (coprolites) but moulds from the digestive tract (cololites) are also recognized. Most of the coprolites probably were produced by deposit-feeding invertebrates but rare specimens dominated by carapace fragments of bradoriid? arthropods are coprolites from predators. Zigzag-folded bromalites are interpreted as cololites of orthothecid hyoliths and are also recognized in inequivalent strata in China. Longitudinally wrinkled forms may be cololites of unknown origin. Minute spheres (Arenigiapella) forming one coprolite are interpreted as microcrystalline phosphatic coatings of bacteria. Post-diagenetic boring attributed to endolithic cyanobacteria is widespread.
机译:来自北格陵兰的寒武纪(系列2和系列3)的六种磷化溴化铝矿组合,使人们对化石组合中的群落结构有了更多的了解,而化石组合中则以微观骨架生物为主。从乙酸残渣中提取的布朗马岩显示出广泛的形态,包括颗粒,分段的杆,起皱的,光滑的和分段的回旋弦。大多数被解释为挤出的粪便材料(共沸石),但也可识别出消化道中的霉菌(共沸石)。大部分共生proprolites可能是由无脊椎动物的饲养饲料产生的,但罕见的标本是由bradoriid的甲壳碎片主导的。节肢动物是来自掠食者的副prolites。之字形折叠的蓝铁矿被解释为正统蛇纹岩的软陶器,并且在中国的不等价地层中也得到认可。纵向起皱的形式可能是来源不明的胶体。形成一种共proprolite的微小球体(Arenigiapella)被解释为细菌的微晶磷酸盐涂层。成岩后的无聊归因于内生的蓝细菌。

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