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Decimetre-scale multicellular eukaryotes from the 1.56-billion-year-old Gaoyuzhuang Formation in North China

机译:中国北方15.6亿年前高玉庄组的十米级多细胞真核生物

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Fossils of macroscopic eukaryotes are rarely older than the Ediacaran Period (635–541 million years (Myr)), and their interpretation remains controversial. Here, we report the discovery of macroscopic fossils from the 1,560-Myr-old Gaoyuzhuang Formation, Yanshan area, North China, that exhibit both large size and regular morphology. Preserved as carbonaceous compressions, the Gaoyuzhuang fossils have statistically regular linear to lanceolate shapes up to 30?cm long and nearly 8?cm wide, suggesting that the Gaoyuzhuang fossils record benthic multicellular eukaryotes of unprecedentedly large size. Syngenetic fragments showing closely packed ~10?μm cells arranged in a thick sheet further reinforce the interpretation. Comparisons with living thalloid organisms suggest that these organisms were photosynthetic, although their phylogenetic placement within the Eukarya remains uncertain. The new fossils provide the strongest evidence yet that multicellular eukaryotes with decimetric dimensions and a regular developmental program populated the marine biosphere at least a billion years before the Cambrian Explosion.
机译:宏观真核生物的化石很少比埃迪卡拉安时期(635-5.41亿年(米尔))更古老,它们的解释仍存在争议。在这里,我们报道了来自华北燕山地区1,560年前的高玉庄组的宏观化石的发现,该化石既具有大尺寸又具有规则的形态。高余庄化石保存为碳质压缩物,统计上呈线形至长披针形的正则线性形状,长至30?cm,宽近8?cm,表明高余庄化石记录了底栖多细胞真核生物,其规模前所未有。同源碎片显示紧密堆积的〜10?μm细胞排列成厚片,进一步加强了解释。与活的拟生物的比较表明,这些生物是光合作用的,尽管它们在真核生物中的系统发育位置仍然不确定。这些新的化石提供了迄今最有力的证据,证明具有十分之一尺度的多细胞真核生物和定期的发育计划至少在寒武纪爆炸发生之前十亿年前就已经遍布海洋生物圈。

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