Thursday, February 14, 2019

Hyolithus: a Cambrian mystery solved

Preliminary comments: The fossil Hyolithus has long been an enigma. Is it a mollusk, a worm, or what? When I first started teaching, it was strongly favored to be an early mollusk. It remained in that uncertain mode until recently when a team of paleontologists (Moysiuk et al., 2017) collected over 1,500 specimens from British Columbia. Remarkable specimens were found that show, for the first time, soft-part anatomy impression. Now the mystery is solved. Read on to found out what the answer is.


Impression of a fossil specimen of the hyolithid Hyolithus cecrops Walcott, 1917 (19 mm height, early middle Cambrian, northwestern Montana). Found with specimens of trilobites [Albertella helena], brachiopods, and trace fossils.

Hyolithids are a group of small, somewhat flat-shaped, shells whose biologic affinities have long been uncertain. The most common assumption was that they were gastropods, which had a planktonic (floating) existence, like the pteropod gastropods (so-called "sea butterflies") found in modern seas. Their most perplexing morphologic feature were the two "oars," which are now named "helens." In the image shown above, only the left helen is preserved.

Most of the several hundred species belong to genus Hyolithus, which had a worldwide distribution, starting in Early Cambrian time. They became diminished during Ordovician and lingered thereafter until the Middle Permian.


Dorsal view of exterior of H. cecrops showing the major morphologic characters.  


Side view of exterior of H. cecrops. The operculum (lid) could open slightly, and the feeding apparatus (probably similar to the lophophore of some modern animals), could then be extended into the water column. The helens were used as stilts/props for holding the animal above the muddy bottom substrate. 

Dorsal view of interior of H. cecrops, showing critically important soft-tissue impressions: the presumed lophophore, the location of the mouth, and the U-shaped gut. These impression are indicative that hyolithids were not planktonic mollusks. Instead, they were benthonic (bottom dwellers) animals that had their closest relatives being the lophophore-bearing brachiopods and bryozoans. 

For more information see:
Moysiuk, J. et al. 2017. Nature v. 54:394–397 (like other pay-for- subscription journals, the abstract is free, but it costs to read or download the actual paper).


Saturday, February 2, 2019

Tektite, an interesting rock

Tektites (pronounced tek-tites) are the by-products of meteorite impacts on Earth.  Composed of gravel-sized, natural glass particles, which are predominantly black, they can also be brown, gray, or green. They made up of natural glass formed from molten terrestrial debris thrown into the air after a meteor strikes the ground. Tektites have no crystalline structure because they cool so rapidly, thus crystals cannot grow. In that sense, they are similar to obsidian (volcanic glass), but tektites have lower water content than obsidian glass.
A tektite (4 cm length) from Guang Dong, Kwangtung Province, China.
Tektites occur within “strewn-fields” associated with meterorite impact craters. Some of the more famous “strewn-fields” are in southern China, the Czech Republic, and the Ivory Coast of Africa (Ghana).


If you check online, you can find tektites for sale, at a modest price in most cases. For more information about tektites, see <www.britannica.com>