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by Elizabeth Pennisi

Notho In my essay on the origin of flowering plants, I discussed many ideas related to how angiosperms came to dominate terrestrial ecosystems. Representing hundreds of thousands of species and 96% of all terrestrial vegetation, flowering plants are the most successful land plants on Earth. Researchers have long chalked it up to their flowers, which enlist insects and other animals to help them reproduce and spread. But two plant biologists credit the leaves instead. More leaf veins (left) made the plants better photosynthesizers, say Timothy Brodribb, a hydraulic physiologist at the University of Tasmania in Australia, and Taylor Feild, now at the University of Tennessee, Knoxville. "The importance of vein density has never before been so clearly presented," says Peter Wilf, a paleobotanist at Pennsylvania State University, University Park. Read about their compelling data and argument here.


Credit: Timothy Brodribb

Tetrahedraletes medinensis(3)No bigger than specks of dust, cryptospores are one of our largest windows into the deep history of plants. These ancient spores and pollen show up in the fossil record between 465 million and 407 million years ago, a key moment for Earth’s greenery. During the first half of that period, the nonvascular land plants—mosses, liverworts, and hornworts—held sway, dominating the landscape for 30 million years. But eventually, vascular plants—ferns and seed-bearing plants—evolved and gradually took over. By examining the shapes and structures of cryptospores collected during oil explorations, paleobotanists have been trying to pin down this transition. New finds now push back the date when vascular plants appeared by almost 30 million years, to about 450 million years ago, Philippe Steemans of the University of Liège, Belgium, and colleagues report in the 17 April issue of Science.

Cryptospores differ from modern spores and pollen in that they come in clumps of two or four, having failed to separate as modern pollen does into individual cells. Thus these dyads and tetrads (above; scale is 10 micrometers) are diagnostic for ancestral land plants. Spores that have disassociated from these clumps represent more modern plants, and folds and bumps on spore surfaces distinguish species and thus are indicative of diversity.

Since 1990, Steemans and Charles Wellman of the University of Sheffield in the United Kingdom have been retrieving fossils from boreholes dug for oil exploration in Saudi Arabia. They dissolve the rock in different solvents to remove carbonate and silicate materials and examine the remaining organic material under light and scanning electroambitisporites avitus(2)n microscopes. They typically find marine fossils, which help them determine the age of the rock, as well as spores and pollen.

In the most recent samples, the cryptospores at first seemed quite ordinary. But when they looked closely, Steemans and Wellman found single spores—called  trilete spores (left; scale is 10 micrometers)—dispersed among the dyads and tetrads. “Our first reaction was to think that the samples had been contaminated by younger material,” Steemans recalls. But an independent analysis in a second laboratory turned up the same ancient trilete spores.

“These generally don’t appear until much later,” about 436 million years ago, says Wellman. Thus these newly described, 450-million-year-old cryptospores “probably represent the origin of vascular plants.”

—Elizabeth Pennisi

Photo Credit: P. Steemans

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