MISSING LINKS AND DAWN MONKEYS
What is unique about this particular ravine, though, is not the loess.
In this part of Shanxi Province, loess is ubiquitous, draping over older
geological features like autumn leaves covering a well-kept lawn. But here,
as the ravine approaches the Yellow River, it cuts deep into the loess. For
the last fifty yards or so of its existence, the ravine finally succeeds in
breaking through the loess altogether to expose the much older underlying
strata. Even to the untrained eye, it is clear that these rocks are different,
both in terms of their composition and their segregation into different
layers or beds. They consist of alternating bands of blue-green
mudstone, pale yellow and white limestone, and thick gray sandstones,
the last of which show internal evidence of stratification in the form of
minute swales of sand grains known as cross-bedding. The fossils we seek
are concentrated in the layers of mudstone and limestone. They are
roughly forty million years old, about six times older than the earliest
putative hominids ever discovered. They pertain to an interval of Earth
history known as the Eocene, the Greek roots of which translate more
or less as “dawn of recent [life].”
As its etymology suggests, the Eocene was a pivotal period in the history
of life on Earth—a time of transition from ancient to modern. The
earliest members of most living orders of mammals first appeared and
became geographically widespread, replacing more archaic forms that
left no living descendants. Such distinctive and highly specialized types
of modern mammals as bats and whales first showed up in the Eocene,
together with the earliest odd-toed ungulates (horses, rhinos, and tapirs),
even-toed ungulates (pigs, camels, and primitive relatives of deer and antelopes),
and others. The order of mammals to which we belong, the Primates,
also first became geographically widespread and ecologically
prominent at the beginning of the Eocene, although a few scattered fossils
hint that primates are somewhat older yet. At the same time, the
Eocene witnessed the decline and extinction of many groups of mam-
In this part of Shanxi Province, loess is ubiquitous, draping over older
geological features like autumn leaves covering a well-kept lawn. But here,
as the ravine approaches the Yellow River, it cuts deep into the loess. For
the last fifty yards or so of its existence, the ravine finally succeeds in
breaking through the loess altogether to expose the much older underlying
strata. Even to the untrained eye, it is clear that these rocks are different,
both in terms of their composition and their segregation into different
layers or beds. They consist of alternating bands of blue-green
mudstone, pale yellow and white limestone, and thick gray sandstones,
the last of which show internal evidence of stratification in the form of
minute swales of sand grains known as cross-bedding. The fossils we seek
are concentrated in the layers of mudstone and limestone. They are
roughly forty million years old, about six times older than the earliest
putative hominids ever discovered. They pertain to an interval of Earth
history known as the Eocene, the Greek roots of which translate more
or less as “dawn of recent [life].”
As its etymology suggests, the Eocene was a pivotal period in the history
of life on Earth—a time of transition from ancient to modern. The
earliest members of most living orders of mammals first appeared and
became geographically widespread, replacing more archaic forms that
left no living descendants. Such distinctive and highly specialized types
of modern mammals as bats and whales first showed up in the Eocene,
together with the earliest odd-toed ungulates (horses, rhinos, and tapirs),
even-toed ungulates (pigs, camels, and primitive relatives of deer and antelopes),
and others. The order of mammals to which we belong, the Primates,
also first became geographically widespread and ecologically
prominent at the beginning of the Eocene, although a few scattered fossils
hint that primates are somewhat older yet. At the same time, the
Eocene witnessed the decline and extinction of many groups of mam-
mals that first evolved alongside the dinosaurs, or immediately following
their demise. Examples include the vaguely rodentlike multituberculates,
the raccoon- or bearlike arctocyonids, and the large herbivores
known as pantodonts and uintatheres. The Eocene also witnessed a great
evolutionary diversification of flowering plants, together with the insects
that feed on them.3
their demise. Examples include the vaguely rodentlike multituberculates,
the raccoon- or bearlike arctocyonids, and the large herbivores
known as pantodonts and uintatheres. The Eocene also witnessed a great
evolutionary diversification of flowering plants, together with the insects
that feed on them.3