Our perception of biodiversity in the geological past is incomplete and biased because most organisms did not have mineralized skeletons and therefore had little chance of fossilization. This especially refers to shal...Our perception of biodiversity in the geological past is incomplete and biased because most organisms did not have mineralized skeletons and therefore had little chance of fossilization. This especially refers to shallow- water marine environments, rarely represented by localities with exceptional preservation of fossil material （known as taphonomic windows or Konservat-Lagerstaitten）. Such extraordinary “windows” may markedly broaden our knowledge of biodiversity of the past. Here, we show a review of the invertebrate fossils from recently discovered locality in the Lower Ordovician Fenxiang Formation of Hubei Province in southern China revealing exceptional preservation of soft tissues. The fauna, generally of shal- low-water aspect, contains linguloid brachiopods with a remarkably preserved pedicle, the oldest traces of nema- tode life activities, the oldest reliable record of hydroids, the first fossil antipatharian corals, a pyritized colonial organism of unknown affinity, supposed arthropod ap- pendages, probable phosphatized scalidophoran worm embryo and other fossils. Our discovery supports the opinion that the famous soft-bodied preservation of Bur- gess Shale- or Chengjiang-type did not vanish from the fossil record in post-Cambrian times. The new finding represents a prelude to the Great Ordovician Biodiversifi- cation Event and provides evidence for calibration of molecular clock of several invertebrate lineages.展开更多
基金supported by the National Science Centre(NCN,Poland)(A.B.,DEC-2012/07/B/NZ8/02701)the National Natural Science Foundation of China(NSFC)(41172001)
文摘Our perception of biodiversity in the geological past is incomplete and biased because most organisms did not have mineralized skeletons and therefore had little chance of fossilization. This especially refers to shallow- water marine environments, rarely represented by localities with exceptional preservation of fossil material （known as taphonomic windows or Konservat-Lagerstaitten）. Such extraordinary “windows” may markedly broaden our knowledge of biodiversity of the past. Here, we show a review of the invertebrate fossils from recently discovered locality in the Lower Ordovician Fenxiang Formation of Hubei Province in southern China revealing exceptional preservation of soft tissues. The fauna, generally of shal- low-water aspect, contains linguloid brachiopods with a remarkably preserved pedicle, the oldest traces of nema- tode life activities, the oldest reliable record of hydroids, the first fossil antipatharian corals, a pyritized colonial organism of unknown affinity, supposed arthropod ap- pendages, probable phosphatized scalidophoran worm embryo and other fossils. Our discovery supports the opinion that the famous soft-bodied preservation of Bur- gess Shale- or Chengjiang-type did not vanish from the fossil record in post-Cambrian times. The new finding represents a prelude to the Great Ordovician Biodiversifi- cation Event and provides evidence for calibration of molecular clock of several invertebrate lineages.
