![]() |
![]() |
EARTH
|
Traditionally it is thought
that the closest living relation to parrots was the Colubiformes but some morphological studies
have placed Psittaciforms
as the sister branch of Coraciiformes or that
of Coliiformes. Furthermore, research from
molecular studies places parrots as the sister taxon of the large clade
comprised of an assemblage of neognath birds, however is widely
accepted that they are
one of the oldest avian orders in modern times.To date, the
majority of palaeontological evidence is based on very few genetic studies. Fossil parrot remains are rare and those that have been identified are
often the subject of much debate. Early Psittaciformes have mainly been found
in the northern hemisphere (Walton-on-the-Naze, England;Messel, Germany, etc.),
with only a few, relatively recent, essentially modern parrot remains being
found within their present range (mainly in tropical and sub-tropical
Australasia and South America). These northern European specimens are thought
to be by some, as a sister clade to modern Psittaciformes as they lack reduced furculas
and the curved bill, but do possess the zygodactyl feet.
The earliest fossil originates from the Early Eocene period approximately 55 million
years ago, however some fragmentary fossils, such as a mandible bone, which
design is only known to be attributed to the Psittaciforme order, dates
from as early as the Late Cretaceous (65 Million years), however whether this
truly represents an early parrot, remains highly controversial.
One could argue
that the reason behind the lack of knowledge concerning Psittaciformes is the
very low fossil number available to work with. There are several reasons for
this low number including the fragility of bird bones (birds have hollow bones)
and the fossilisation process itself. It is unlikely that terrestrial
environments like subtropical forests and the lifestyle of arboreal birds would
allow for the fossilisation process to occur after death. Sites with high
success rate of fossilisation will be normally be of an aquatic environment
with unusual sedimentary deposition rate, such as the Messal oil shale's of
Germany. In the fact that majority of Avifauna fossils are represented by
aquatic/semi aquatic species.
| Million years | Epoch | Name of fossil found | Location | |
| 0.15 - 0.0 Ma | Holocene | Lophopsittacus mauritianus | Mauritius | |
| 1.8 - 0.15 Ma | Pleistocene | Rhynchopsitta phillipsi (Late Pleistocene) | Mexico | |
| 1.4 - 1.8 Ma | Pliocene | Nandayus vorohuenseis (Late Pliocene) | Buenos Aires Province, Argentina | |
| 23.7 - 1.4 Ma | Miocene | Cacatua ??? (Early Miocene) Archaeopsittacus verreauxi |
Queensland, Australia Verreaux, France |
|
| 36.6 - 23.7 Ma | Oligocene | |||
| 57.8 - 36.6 Ma | Eocene | Qeurcypsitta ivani and sundrei (Upper Eocene) Psittacopes lepidus (Mid Eocene) Pulchrapollia gracillis (Lower Eocene) |
Phoshorites dy Quercy, France Messel, Germany London Clay, Essex Britain |
|
| 65 - 57.8 Ma | Palaeocene | None recorded | ||
| 144-65 Ma | Cretaceous | Parrot mandible???, Loriidae? | Lance Formation- Wyoming USA | |