Sea Creature Fossils Reveal Prehistoric Division of Labor
Ancient colonies of plankton were surprisingly good at cooperation, according to a new look at a very old fossil.
The slab of rock preserves the remains of a graptolite colony, which leaves fossils that look almost like hieroglyphics etched in stone. Graptolites were early animals that first arose nearly half a billion years ago. They almost entirely died out at the end of the Ordovician period about 443 million years ago. While no graptolites survive today, scientists believe they are most closely related to an unusual group of worm-like animals called pterobranches, which build and live in tubes on the ocean floor.
Just as modern coral leave behind amazing structures when they die, graptolites left behind the skeletons of their homes when they went extinct. These fossils are common, but it wasn't until University of Leicester geologist Jan Zalasiewicz was examining a museum specimen that he noticed something strange: The connections between different parts of the colony were not identical.
"The light caught one of the fossils in just the right way, and it showed complex structures I had never seen in a graptolite before," Zalasiewicz said in a statement. "It was a sheer stroke of luck … one of those eureka moments."
In some parts of the colony, Zalasiewicz said, the connections between individual animals looked like "slender criss-crossing branches." Others had odd hourglass shapes. Zalasiewicz and his colleagues reported the discovery online Aug. 9 in the journal Geological Magazine.
These fossil remnants suggest that graptolite colonies featured a division of labor, Zalasiewicz said, with some individual animals responsible for feeding and others for building. (Graptolites sported long, tentacled arms for feeding.)
"This amazing fossil shows sophisticated prehistoric cooperation, preserved in stone," he said.
- Deep-Sea Creepy-Crawlies: Images of Acorn Worms
- Dangers in the Deep: 10 Scariest Sea Creatures
- Strange Coral: A Gallery of Sea Pens
Copyright 2012 LiveScience, a TechMediaNetwork company. All rights reserved. This material may not be published, broadcast, rewritten or redistributed.