Eocene
Introduction
The Eocene epoch extends from 55.8 to 33.9 million years ago. Eocene
is derived from Greek and means "dawn of the modern". This name is
well chosen as representatives of most modern orders of birds and mammals
appear during this epoch.
Primary
Producers & Reefs
Coccolithophorids experienced a mass extinction
at the K/T boundary. Diatoms and dinoflagellates were less affected.
By the Eocene all three groups had recovered; however, from then
on dinoflagellate and coccolithophore diversity declined. Diatoms,
on the other hand, have increased in diversity. Today, diatoms are
the most diverse group in the plankton.
Interestingly,
the success of diatoms may be tied to the evolution of grasses.
Grasses sequester
silica into their tissues in the form of phytoliths. Phytoliths
add structural support to the plant. Phytoliths may also
produce a gritty
texture making the plant distateful to herbivores. The Silica
released from phytoliths during plant
decay is easily dissolved in water and washed in rivers and
seas. The influx of phytolith silica into
the oceans would benefit diatoms as they construct their
frustules from silica. Increase in diatom diversity and abundance
is correlated with the appearance of phytoliths during the
Late Cretaceous and with the expansion of grasses in the
Eocene, Oligocene and Middle Miocene (Kooistra, Gersonde,
Medlin & Mann, 2007, pp. 228 & 229). Diatoms,
dinoflagellates, and coccolithophores make up the dominant
primary producers in todays oceans.
Marine
Invertebrates
Fish
Amphibians
Reptiles
Mammals
Birds
Insects
Plants
Grube Messel
Grube
Messel or the Messel Pit is a Fossil Laggerstaten near the town
of Messel, Germany that was declared a UNESCO World Heritage
Site in 1995. From 1875 to the 1960's the site was developed
as an open pit oil shale mine. Over the years many fossils were
found during the mining operations. The sediments that formed
Grube Messel were layed down in a restricted lake basin within
the Rhine Rift Valley during the Early Eocene 49 million years
ago. Faulting and volcanic activiey were common within this rift
valley. The Grube Messel stratigraphy and biota
suggest the basin was part of a lush subtropical environment
with extensive rivers and lakes. Some interpret the deposit as
representing a crater lake. The
flora and fauna preserved in the Messel shale represent a number
of environments that surrounded the lake including: open water,
swamp, bank-side, damp forest and drier elevated regions.
Among
plants angiosperms or the flowering plants are the most common
at Messel; although, gymnosperms and ferns are also present.
Ferns, swamp cypresses, grasses (such as rushes and sedges),
lilies, palms, laurels, tea,
grapevines, citrus, and walnut represent environments that
were inundated with water or moist. Pines, beeches, chestnuts,
and
oak grew in drier conditions farther from the lake.
Among
arthropods beetles are the most common and beautiful in the Messel
shale. Click beetles, weevils, jewel, dung, stag, water,
longhorn, rove and leaf beetles are represented. The larvae of
a particular genus of water beetle Eubrianax are interesting
because extant forms live in waterfalls were oxygen levels are
high. The elytra or wing cases of some beetle specimens exhibit
a colorful
iridescence.
Baltic
Amber
Green
River Formation
Florissant
|
Bibliography |
Kooistra,
W.H.C.F., Gersonde, R., Medlin, L. K. & Mann, D.G. (2007).
The Origin and Evolution of the Diatoms: Their Adaptation
to a Planktonic Existence. In Falkowski, P.G. Knoll, A.H.
[Eds] Evolution of Primary Producers in the Sea.
(pp. 133-163). China: Elsevier Academic Press. |