-40%

Rare coal age pre dinosaur fossil plant early cycas ancestor Callipteridium

$ 32.73

Availability: 100 in stock
  • All returns accepted: Returns Accepted
  • Return shipping will be paid by: Buyer
  • Item must be returned within: 30 Days
  • Condition: New
  • Restocking Fee: No
  • Modified Item: No
  • pre dinosaur fossil: fossil plant
  • Refund will be given as: Money back or replacement (buyer's choice)

    Description

    My specimens are gunine and will be delivered with a "Certificate of authenticity, age and origin"  and scientific papers allowing plant identification !
    I combine shipping costs.
    Each item is different, so please wait with payment after purchase -
    I will send You a combine invoice.
    Usually, it will be cost of shipping the heaviest item.
    Specimen:       Rare, nicely definied fossil plant specimen - early cycas ancestor
    Callipteridium striatum
    WAGNER
    Locality:
    All detailed and accurate data will be provided with the specimen
    Stratigraphy:
    Upper Carboniferous - Late
    Pennsylvanian
    - Stephanian A
    Age:
    ca. 302 - 300 Mya
    Matrix dimensions:
    ca. 10 x 8,5 x 1,0 cm ( white square on pictures is 1,0 x 1,0 cm)
    Description:
    Here is a rare, very nice classic Stephanian - late Upper Carboniferous fossil plant specimen - early cycas ancestor belonging to
    Peltaspermales -
    Callipteridium striatum
    WAGNER
    Callipteris and Callipteridium
    is a widely used historical morphogenus for late Paleozoic ( mostly permian !!! ) foliage attributed to peltasperms.
    The peltaspermales were initially described from Mesozoic based on associated foliage, pollen and seed- bearing parts ( Thomas, 1933; Harris 1937).
    Today this enigmatic plants order incorporates specimens ranging from Pennsylvanian ( Kerp et al. 2001) to Triassic. Many of them are know almost exclusively from Permian. There is not a great deal of detailed information known about the pollen organg of the peltasperms. In the more primitive forms , it appears that the polen organs are pinnately organized. At the present time , the Peltaspermales are perhaps the most confounding of all of plants. Moreover, the pollen organs assigned to Autunia bear bisaccate grains of the
    Veicaspora
    type, whereas those known from
    Antevsia
    are monosculate and conform to
    Cycadopites
    .