This is a time of continents colliding, North America and Greenland hitting Europe, smashing together and making mountains. The planet鈥檚 land mass is mostly dusty and barren. Rivers were more like great expanses of water sliding into the ocean.
鈥淵ou鈥檇 hardly know the place,鈥 says Martin Gibling, professor with 麻豆传媒鈥檚 Department of Earth Sciences. 鈥淭here was bare rock and sand, with crusts of bacteria and algae over the rock surfaces. And ancient rivers were very different, like big sheets of water carrying sand and gravel. They weren鈥檛 like channels whatsoever.鈥
Dr. Gibling and postdoctoral researcher Neil S. Davies wanted to find out more about those big rivers. What happened during the evolution of the Earth to throw them for a loop?
鈥淚f you think of a river, it鈥檚 wavy, it鈥檚 meandering,鈥 explains Dr. Gibling. 鈥淎 river has curves, eroding into its bank on one side, and depositing sediments on the other.鈥
For the answers to one of the most significant environmental changes in the Earth鈥檚 history, they turned to the fossil record using a literature compilation and fieldwork. Their research took them to 35 sites around the globe, including Port-au-port, Newfoundland, the Gasp茅 Peninsula of Quebec, the Channel Islands off the coast of France and Death Valley in California.
The difference, they discovered, came with the earliest plants. By stretching their roots down, they stabilized river banks. Instead of wide and sheet-like, rivers evolved to become more confined and narrower. Their research, highlighting the co-evolution of land plants and river landscapes, has just been published in the journals Geology and Earth-Science Reviews.
鈥淥nce the plants started to get a toehold, they sent spores into more inland areas,鈥 says Dr. Davies, who hails from Birmingham, England. 鈥淭he entire process took about 50 million years, with vegetation spreading until it dominated every landscape except total desert. The Earth could never be the same again.鈥
SEE: 鈥溾 in Earth-Science Reviews, February 2010
鈥溾 in Geology, January 2010