Picture of Aphantomartus pustulatus, a 300-million-year-old fossil trigonotarbid from the 7-11 Mine in Ohio that was immersed in water to contrast the body outline with the surrounding rock matrix. The fossil was collected by Gregory McComas, an avid fossil collector and geology graduate of Youngstown State University in Ohio, and studied by Cary R. Easterday, a master's degree student in the Department of Geological Sciences at Ohio State University. Easterday found evidence that these long-extinct arachnids may have been able to spin silk like modern spiders. Photo by Cary R. Easterday, courtesy of Ohio State University.
Interpretive drawing of Aphantomartus pustulatus, a 300-million-year-old fossil trigonotarbid from the 7-11 Mine in Ohio, showing surface details and outline of the body. An arrangement of tiny bumps called a 'microtubercle row' are found along the hind legs that are similar in shape and location to a calamistrum, a structure found in some modern spiders that is used to spin silk. Drawing by Cary R. Easterday, courtesy of Ohio State University.
Picture of Aphantomartus pustulatus, a 300-million-year-old fossil trigonotarbid from the 7-11 Mine in Ohio that was whitened with ammonium chloride to show surface details on the body. The fossil was collected by Gregory McComas, an avid fossil collector and geology graduate of Youngstown State University in Ohio, and studied by Cary R. Easterday, a master's degree student in the Department of Geological Sciences at Ohio State University. Easterday found evidence that these long-extinct arachnids may have been able to spin silk like modern spiders. Photo by Cary R. Easterday, courtesy of Ohio State University.
SEM micrograph of Aphantomartus pustulatus, a 300-million-year-old trigonotarbid from the 7-11 Mine in Ohio, showing the 'microtubercle row' on the patella of the fourth walking leg (left side). A row of tiny bumps is clearly visible. Cary R. Easterday, a master's degree student in the Department of Geological Sciences at Ohio State University, said this configuration of microtubercles is highly unusual, suggesting a highly specialized function. This microtubercle row is similar in shape and location to the calamistrum of some modern spiders and may be evidence of silk-spinning in this long-extinct creature. SEM micrograph by Sreenivas Bhattiprolu, electron microscopist and microprobe analyst at Ohio State, courtesy of Ohio State University.
SEM micrograph and interpretive sketches of Aphantomartus pustulatus, a 300-million-year-old fossil trigonotarbid from the 7-11 Mine in Ohio, showing the distribution of microtubercles (tiny bumps) on the abdomen. Cary R. Easterday, a master's degree student in the Department of Geological Sciences at Ohio State University, said that microtubercles located on the trigonotarbid abdomen probably were not used for silk-spinning, but served other functions. Most likely, they were attached to tactile hairs used to sense the surrounding environment, as seen in "hairy" spiders today. SEM micrograph by Sreenivas Bhattiprolu, electron microscopist and microprobe analyst at Ohio State. Interpretive sketches by Cary R. Easterday, courtesy of Ohio State University.

 

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