Set number: 1881

  • Davidhakania imbriei VR 1560 1
  • Davidhakania imbriei VR 1572 2
  • Davidhakania imbriei VR 1575 3
  • Davidhakania imbriei VR 1565 4
  • Davidhakania imbriei VR 1561 5
  • Davidhakania imbriei VR 1571 6
  • Davidhakania imbriei VR 1573 7
  • Davidhakania imbriei VR 1566 8
  • Davidhakania imbriei VR 1553 9
  • Davidhakania imbriei VR 1552 10
  • Davidhakania imbriei VR 1554 11
  • Davidhakania imbriei VR 1588 12
  • Davidhakania imbriei VR 1557 13
  • Davidhakania imbriei VR 1559 14
  • Davidhakania imbriei VR 1558 15
  • Davidhakania imbriei VR 1589 16
  • Davidhakania imbriei VR 1598 17
  • Davidhakania imbriei VR 1595 18
  • Davidhakania imbriei VR 1603 19
  • Davidhakania imbriei VR 1586 20
  • Davidhakania imbriei VR 1590 21
  • Davidhakania imbriei VR 1604 22
  • Davidhakania imbriei VR 1596 23
  • Davidhakania imbriei VR 1585 24
  • Davidhakania imbriei VR 1591 25
  • Davidhakania imbriei VR 1578 26
  • Davidhakania imbriei VR 1587 27
  • Davidhakania imbriei VR 1582 28
  • Davidhakania imbriei VR 1592 29
  • Davidhakania imbriei VR 1579 30
  • Davidhakania imbriei VR 1593 31
  • Davidhakania imbriei VR 1581 32
    10µm
Moscow Landing, bank of the Tombigbee River, Alabama, USA

In the mobile mount

Set number: 1879

  • Davidhakania imbriei VR 462 1
  • Davidhakania imbriei VR 458 2
  • Davidhakania imbriei VR 466 3
  • Davidhakania imbriei VR 472 4
  • Davidhakania imbriei VR 463 5
  • Davidhakania imbriei VR 459 6
  • Davidhakania imbriei VR 467 7
  • Davidhakania imbriei VR 473 8
  • Davidhakania imbriei VR 470 9
  • Davidhakania imbriei VR 469 10
  • Davidhakania imbriei VR 468 11
  • Davidhakania imbriei VR 474 12
    10µm
Moscow Landing, bank of the Tombigbee River, Alabama, USA
Final Epithet
Davidhakania imbriei (Haq & Lohman, 1976) Varol, 2025a
Basionym

Neochiastozygus imbriei Haq & Lohman, 1976

Remarks

This species of Davidhakania is characterised by an asymmetrical diagonal cross, with its acute angle aligned along the long axis of the discolith. The longer arm is inclined less than 20° (often less than 10°) counterclockwise relative to the long axis of the discolith on the distal side. Its optical properties are consistent with those of the genus Davidhakania. This species exhibits extinction lines with a typical extinction angle of approximately 74° on the distal side and displays length-fast (-) elongation.

Davidhakania imbriei differs from Davidhakania eosaepes in the alignment of the longer arm of the crossbar. In Davidhakania imbriei, the longer arm is inclined less than 20° counterclockwise relative to the long axis of the discolith on the distal side, whereas in Davidhakania eosaepes, it is inclined more than 20°.

Davidhakania eosaepes is further distinguished by its asymmetrical crossbar, whereas Davidhakania saepes and Davidhakania partingtonii possess symmetrical crossbars.

References

Haq, B. U. & Lohmann, G. P. 1976. Early Cenozoic calcareous nannoplankton biogeography of the Atlantic Ocean. Marine Micropaleontology. 1: 119-194.

Varol, O. 2025a. A practical guide to optical studies of calcareous nannofossils. Grzybowski Foundation Special Publication. 29: 1-222