
Dr. Rowan Martindale, a paleoecologist and geobiologist at the University of Texas at Austin, was hiking through the Dadès Valley in Morocco’s Central High Atlas Mountains when something unusual caught her attention and made her stop.
Martindale and her research team, including Stéphane Bodin of Aarhus University, were exploring the rugged valley to study the ecology of ancient reef systems that once existed there when the area lay beneath the ocean. Reaching those reefs required crossing numerous layers of turbidites, sediments formed by dense underwater debris flows. Ripple patterns often appear on these deposits. However, Martindale noticed small ridges and wrinkles layered on top of the ripples that seemed unusual.
“As we’re walking up these turbidites, I’m looking around and this beautifully rippled bedding plane caught my eye,” says Martindale. “I said, ‘Stéphane, you need to get back here. These are wrinkle structures!'”
What Are Wrinkle Structures
Wrinkle structures are tiny ridges and pits ranging from millimeters to centimeters across. They develop when algae and microbial communities grow in mats across sandy seafloors. These delicate textures are rarely preserved in younger rocks because animals often disturb and destroy them. As a result, wrinkle structures are uncommon in rocks younger than about 540 million years old, when animal life rapidly diversified and began actively stirring ocean sediments.
Today, scientists typically find wrinkle structures in shallow tidal environments where sunlight supports photosynthetic algae.
Why These Wrinkles Should Not Exist
The wrinkle structures Martindale spotted appeared in rocks that formed far below the ocean surface. The turbidites where they were found had been deposited at depths of at least 180 meters, far too deep for sunlight to penetrate. This meant the structures could not have formed from the same sunlight dependent algae that create wrinkle patterns in shallow environments today.
Previous claims of wrinkle structures in deep water turbidite deposits have also been disputed. Another complication was the age of the rocks. At about 180 million years old, they formed during a time when animals were actively disturbing the seafloor worldwide, which normally erases delicate microbial textures. In other words, the wrinkle structures Martindale saw should not have been preserved at all.
Recognizing how unusual the find was, she set out to confirm whether her first impression was correct.
“Let’s go through every single piece of evidence that we can find to be sure that these are wrinkle structures in turbidites,” says Martindale, because wrinkle structures, usually photosynthetic in origin, “shouldn’t be in this deep-water setting.”
Evidence of Chemosynthetic Microbial Life
The research team carefully examined the surrounding rock layers and confirmed that the sediments were indeed turbidites. Next they investigated whether the unusual textures truly formed from biological activity.
Chemical testing provided a key clue. The sediment just beneath the wrinkles contained elevated carbon levels, which often indicate a biological origin. The team also looked to modern ocean environments for comparison. Footage from remotely operated submersibles exploring seafloors far below the photic zone revealed that microbial mats can develop there as well, but they are produced by chemosynthetic bacteria. These microbes obtain energy from chemical reactions instead of sunlight.
How Deep Sea Microbes Created the Wrinkles
By combining geological observations, chemical evidence, and modern examples from the deep ocean, the scientists concluded that they had discovered chemosynthetic wrinkle structures preserved in the rock record.
Turbidite flows likely played a critical role in creating the right conditions. These debris flows transport nutrients and organic material into deep water while also lowering oxygen levels in the surrounding sediments. Such conditions can support communities of chemosynthetic bacteria.
During quieter periods between debris flows, these bacteria can spread across the seafloor and form mats on top of the sediment. As the mats grow, they develop the wrinkled surface patterns that Martindale observed in the rocks of Morocco. In most cases, the next debris flow would erase the mat, but occasionally the structure becomes buried and preserved.
Expanding the Search for Ancient Life
Martindale now hopes to conduct laboratory experiments to better understand how wrinkle structures might develop within turbidite environments. She also hopes the discovery encourages scientists to rethink the long standing assumption that wrinkle structures are created only by photosynthetic microbial mats.
If chemosynthetic mats can also produce these features, geologists may begin searching for wrinkle structures in environments that were previously overlooked in the hunt for ancient life.
“Wrinkle structures are really important pieces of evidence in the early evolution of life,” says Martindale. By ignoring their possible presence in turbidites, “we might be missing out on a key piece of history of microbial life.”


















