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Cambrian suspension-feeding tubicolous hemichordates

机译:寒武纪悬浮饲料微管状的高铁酸盐

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The combination of a meager fossil record of vermiform enteropneusts and their disparity with the tubicolous pterobranchs renders early hemichordate evolution conjectural. The middle Cambrian Oesia disjuncta from the Burgess Shale has been compared to annelids, tunicates and chaetognaths, but on the basis of abundant new material is now identified as a primitive hemichordate. Notable features include a facultative tubicolous habit, a posterior grasping structure and an extensive pharynx. These characters, along with the spirally arranged openings in the associated organic tube (previously assigned to the green alga Margaretia), confirm Oesia as a tiered suspension feeder. Increasing predation pressure was probably one of the main causes of a transition to the infauna. In crown group enteropneusts this was accompanied by a loss of the tube and reduction in gill bars, with a corresponding shift to deposit feeding. The posterior grasping structure may represent an ancestral precursor to the pterobranch stolon, so facilitating their colonial lifestyle. The focus on suspension feeding as a primary mode of life amongst the basal hemichordates adds further evidence to the hypothesis that suspension feeding is the ancestral state for the major clade Deuterostomia.
机译:蠕虫状肠神经的化石记录很少,它们与微管翼状支的差异相结合,使早期半酸盐的进化推测成为可能。伯吉斯页岩中的寒武纪奥伊斯亚分离岩已被与类人猿,被膜和cha蛇进行了比较,但是基于大量的新材料,现在被认为是原始的半酸盐。显着特征包括兼性肾小管性习惯,后握结构和广泛的咽部。这些特征以及相关有机管(以前分配给绿藻玛格丽特)中螺旋排列的开口,证实了Oesia是一种分层悬浮喂食器。捕食压力的增加可能是向动物史过渡的主要原因之一。在冠状肠腔中,伴有管子丢失和g条减少,相应地转移了沉积物进食。后部抓握结构可能代表了支的祖先,因此有利于它们的殖民地生活方式。对悬浮饲料的研究是基础半血统中主要的生活方式,这为悬浮饲料是主要进化枝氘代的祖先状态的假说提供了进一步的证据。

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