Sсiеntifiс Аmеricаn (2019-06)

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June 2019, ScientificAmerican.com 29

the communities of animals and plants that live on
open surfaces differ from those that occupy these
more hidden areas such as caves, crevices or under­
hangs. Our Ediacaran fossil discoveries indicate that
this distinction is as old as animal reefs themselves.
These observations are significant because reef
building represents an important ecological innova­
tion. By growing closely together and even cementing
to one another, individuals can become mechanically
stronger, rise above the seafloor away from competi­
tors, enhance feeding efficiency and gain protection
from predators. Like the earliest skeletons, then, the
appearance of reefs in the Ediacaran fossil record may
signal rising, complex ecological pressures. The Cam­
brian explosion, and indeed an arms race between
predator and prey, had already begun.

THE EDIACARAN WORLD
by the mid­ 2010 s it was becoming clear that the Cambri­
an did not mark the sudden, dramatic departure from

the Ediacaran that experts long envisioned. Not only
had researchers begun to amass evidence that animals
started evolving skeletons and building reefs earlier
than traditionally thought, but we had also developed
ecosystem models showing that Ediacaran animal
communities shared many ecological traits with Cam­
brian ones. The “explosion,” we were learning, had a far
longer fuse than was previously recognized.
Then, a few years ago, some key discoveries in Sibe­
ria and China blurred the Ediacaran and Cambrian
worlds even further. A group of researchers from China
and Germany found that Cloudina persisted into the
Cambrian. And my group, together with colleagues
from Russia and China, found fossils long thought to
be unique to the Cambrian in Ediacaran rocks. These
findings underscored to us that to solve the mystery of
the Cambrian explosion we had to figure out the
dynamics of the Ediacaran world in which these ani­
mals originated.
SOURCE: “INTEGRATED RECORDS OF ENVIRONMENTAL CHANGE AND EVOLUTION CHALLENGE THE CAMBRIAN EXPLOSION,” BY RACHEL WOOD ET AL., IN The possible role of shifting oxygen availability is

NATURE ECOLOGY & EVOLUTION

, VOL. 3; APRIL 2019

Illustration by Franz Anthony ( fossils)

Carbon Isotope Variations

12
8
4
0
-4
-8
-12

Ocean Chemistry
Over Space and Time

High

Shallow

Deep

Low

Mean

Millions of Years Ago: 660 640 620 600 580 560 540 520 500


Millions of Years Ago:


480

Cryogenian Ediacaran Fortunian

CAMBRIAN

PALEOZOIC
PROTEROZOIC

PRECAMBRIAN

Oxygen-rich
Iron-rich, oxygen-deficient water (tan) water (blue)

Regional variability (dots)

Widespread (solid)

Oxygen-rich water (blue)

Uncertain Uncertain Uncertain

Hydrogen sulfide–rich
water (red)

Lantianella laevis
Treptichnus pedum (trace fossil)

Charnia masoni

660 640 620 600 580 560 520 500

Cloudina

Ice ages

Fossil Evidence
Surprisingly sophisticated Ediacaran creatures include
Lantianella laevis, a possible forerunner of today’s
jellies; Charnia masoni, which appears to have grown
rooted to the seafloor and absorbed nutrients from
the surrounding water; Cloudina, one of the earliest
animals with a skeleton; and Treptichnus pedum, the
name given to the distinctive traces left behind by an
unknown burrowing animal.

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