Oolites

Click to view larger image of the Utah's Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova
Utah’s Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova

Hi, this is Mark Larese-Casanova from the Utah Master Naturalist Program at Utah State University Extension.

Imagine if prehistoric brine shrimp were responsible for one of the finest examples of architecture in Salt Lake City today.

Okay, so it may be a bit of a stretch, but let me explain. In a previous episode of Wild About Utah, I discussed the life cycle of brine shrimp and the important role that they play in the Great Salt Lake Ecosystem. Well, as the billions of brine shrimp feed on bacteria in Great Salt Lake, they excrete waste in the form of tiny fecal pellets. These pellets, along with sand grains and other bits of debris, eventually settle to the bottom of Great Salt Lake.

In shallow areas of the lake, where wind and waves routinely mix the water, these small particles gradually accumulate layers of calcium carbonate, forming an oolite (spelled o-o-l-i-t-e). This is very similar to how a pearl, also layers of calcium carbonate around a small particle, is formed within the shell of an oyster or mussel. The main difference, aside from a pearl being much larger, is that oolites are typically oblong, rather than round. The beaches on the west side of Antelope Island are a great place to find oolitic sand, which will look and feel as though you have a handful of tiny pearls.

Click to view larger image of the Utah's Oolitic Sandstone, Photo Courtesy and Copyright Mark Larese-Casanova
Utah’s Oolitic Sandstone
Photo Courtesy & Copyright
Mark Larese-Casanova

Around 50 million years ago, large fresh- and salt-water lakes covered parts of Utah, and in these areas, vast amounts of sediments, including oolites, were deposited. Over time, these oolites were compressed and cemented together into limestone.

A quarry near Ephraim in Sanpete County supplied oolitic limestone for the construction of the Governor’s Mansion in 1902 and the original Salt Lake City Public Library in 1905. The Library building, located at 15 South State Street, eventually housed the Hansen Planetarium and is now home to the O.C. Tanner flagship store. The building underwent an extensive restoration just a couple of years ago, and now serves as a shining example of neoclassical architecture in our capitol city.

The truth is, there are tens of millions of years separating oolitic limestone from our modern-day brine shrimp. So, we can’t exactly say that prehistoric brine shrimp were responsible for the existence of the O.C. Tanner building. But, it’s fun to imagine precious gems from around the world housed in a beautiful building constructed from the ‘pearls’ of Great Salt Lake.

Click to view larger image of the historic OC Tanner building made from oolitic sandstone (This building formerly housed the Salt Lake Library and Hansen Planetarium), Photo Courtesy and Copyright Mark Larese-Casanova
Historic OC Tanner Building
(formerly the Salt Lake Library
and later the Hansen Planetarium)
Photo Courtesy & Copyright
Mark Larese-Casanova

For Wild About Utah, I’m Mark Larese-Casanova.
Credits:

Images: Courtesy and copyright Mark Larese-Casanova

Text:     Mark Larese-Casanova, Utah Master Naturalist Program at Utah State University Extension.
Additional Reading:

Utah Geological Survey https://geology.utah.gov/utahgeo/rockmineral/collecting/oolitic.htm

Utah Division of Wildlife Resources, Great Salt Lake Ecosystem Program
https://wildlife.utah.gov/gsl/facts/oolitic_sand.php

Salt Lake Brine Shrimp, https://saltlakebrineshrimp.com/harvest/

Utah at the Smithsonian

Utah at the Smithsonian: Click for a larger view of Diplodicus, Courtesy NMNH.si.edu, Michael Brett Surman, Photographer
Diplodicus
Courtesy NMNH.si.edu
Michael Brett Surman, Photographer

Utah at the Smithsonian: Camarasaurus, Camarasaurus lentus (Marsh), Courtesy https://www.nmnh.si.edu/, Michael Brett Surman, PhotographerCamarasaurus
Camarasaurus lentus (Marsh)

Courtesy NMNH.si.edu
Michael Brett Surman, Photographer

Utah at the Smithsonian: Smithsonian Butte, Public Domain, Courtesy National Scenic Byways Online, https://www.byways.org/ and Bureau of Land Management, John Smith, Photographer

Smithsonian Butte
Public Domain, Courtesy
National Scenic Byways Online and Bureau of Land Management.
John Smith, Photographer

Hi, I’m Holly Strand from the Quinney College of Natural Resources at Utah State University.

You don’t have to be in Utah to appreciate some of its treasures. Examples of Utah natural history can be found in museums around the globe. The last time I was in Washington DC, I explored the collections of the Smithsonian Museum of Natural History. There turned out to be a whole lot more Utah stuff than I ever imagined.

Many would consider dinosaurs to be our most illustrious museum export. Indeed a 90-foot long Utah diplodocus is the centerpiece of the museum’s Dinosaur Hall.

Not far away is an amazingly intact Camarasaurus from Utah’s Dinosaur National Monument. Its fossilized bones remained in position for over 150 million years. So beautifully and naturally preserved, it still rests on part of the sandstone block in which it was found.

Only a tiny fraction of the Museum’s collections are on display. The vast majority of its 126 million specimens are in drawers, vaults, and freezers. These items are meticulously cataloged and preserved and they serve as primary reference materials for researchers around the world. I found many 1000s of cataloged items for Utah plants, mammals and birds. Less abundant, there are still 100s of records representing specimens of our amphibians, reptiles and fish.

If you poke around in the collections databases you are sure to find something of interest. I found records of some 300 Utah plant specimens collected by Lester Frank Ward, a botanist who worked for John Wesley Powell on his western expeditions. Powell also contributed to the Smithsonian’s collection of flora and fauna. I found 8 bison skulls and one grass species, but there is probably more.

There is the skull and partial skeleton of a grizzly killed in Logan Canyon. Not Old Ephraim–his skull is here in Utah–but another one killed the year before.

In 1950, a meteorite struck a driveway just a few feet from a Box Elder County woman. A few years later, the meteorite was donated to the Smithsonian. But not before it was enhanced by local schoolchildren using crayons of various colors.

The museum’s mineral collection contains 1000s of Utah specimen, some with very strange names : I found Beaverite, Rabbitite Englishite, Coffinite, Psuedowavellite, Cristobalite, Alunite, Apatite and even Bieberite. As in Justin, I guess.

Anyway, you get the idea. The Smithsonian collections form the largest, most comprehensive natural history collection in the world. And Utah is a prime contributor of both collection items and the stories behind them.

By the way, not only are Utah things in the Smithsonian, but there are also Smithsonian things in Utah.

For example, the Henry Mountains in south central Utah were named after the first Secretary of the Smithsonian Institution Joseph Henry.

Another example is Smithsonite–or zinc carbonate–which was first identified by James Smithson in 1802. The very same Smithson left his fortune to the United States government, directing that it be used to create the Smithsonian Institution. The mineral Smithsonite has been found in Tooele and Washington Counties.

Lastly, there’s Smithsonian Butte. When the Powell Expedition traveled through the Zion area, geologist Edward Dutton named the Butte after the expedition’s most generous sponsor. Smithsonian Butte Road is a designated national backcountry byway, crossing over the Vermilion cliffs between Utah 9 and Utah 59.

For pictures, sources and links, go to www.Wildaboututah.org

For Wild About Utah, I’m Holly Strand.

Credits:

Images: Information and photos provided with the permission of the National Museum of Natural History, Smithsonian Institution, 10th and Constitution Ave. N.W., Washington, DC 20560-0193. (https://www.nmnh.si.edu/)
Smithsonian Butte, Public Domain, Courtesy National Scenic Byways Online and Bureau of Land Management., John Smith, Photographer
Text: Holly Strand

Sources & Additional Reading


Panoramic Virtual Tour of the Smithsonian National Museum of Natural History (NMNH). Navigate or go directly to the Dinosaur Hall to see the diplodocus from Utah. (Fossils: Dinosaur 2)
https://www.mnh.si.edu/panoramas/index.html

Dinosaur page of the NMNH.https://paleobiology.si.edu/dinosaurs/index.html

Research and Collections of the Smithsonian NMNH.
https://www.mnh.si.edu/rc/

Access to Smithsonian NMNH Museum Collection Records databases
https://collections.mnh.si.edu/search/

Smithsonite, Museum of Natural History, Smithsonian Institute, https://www.mnh.si.edu/onehundredyears/featured_objects/smithsonite.html

Lichens

Click for a larger view of Lichens, Courtesy and copyright 2013 Andrea Liberatore, Photographer
Boulder covered in a
variety of lichen species
Copyright 2013
Andrea Liberatore, Photographer

Click for a larger view of Rosette Lichen, Courtesy and copyright 2013 Andrea Liberatore, PhotographerRosette Lichen
Physcia dubia
Lives in both Antarctica
and the Mojave Desert
Copyright 2013
Andrea Liberatore, Photographer

Click for a larger view of Rim Lichen, Courtesy and copyright 2013 Andrea Liberatore, PhotographerRim Lichen
Lecanora muralis
Has anti-cancer and
anti-microbial properties
Copyright 2013
Andrea Liberatore, Photographer

Click for a larger view of Lichens, Courtesy and copyright 2013 Andrea Liberatore, PhotographerGarovagis Rim Lichen
Leconara garovagii
Used in perfume & sunscreen
Copyright 2013
Andrea Liberatore, Photographer

This spring I visited Red Butte Gardens in Salt Lake City for the first time. My favorite part was a small and very non-descript garden, tucked alongside a walkway and devoted to an organism that isn’t a plant at all, but instead a very under-appreciated genera of life – the lichen.

Lichens are those colorful crusts found growing on rocks and trees, and while sometimes plant-like in appearance, they are not plants. Lichens have no leaves, stems, roots, or vascular systems. Even more strange, lichens are not a single organism, but instead a partnership between two organisms: a fungus and an algae or cyanobacteria. Because the fungus is generally the dominant partner, lichens are classified as members of the Fungus kingdom.

The partnership exhibited by these two organisms is an example of mutualism – a relationship where both parties benefit in some way through their interaction. In this case, the fungus provides a safe and secure home for the alga or cyanobacteria, which in return photosynthesizes and provides the fungus with nutrients. Cyanobacteria and algae are typically found in water and are prone to drying when exposed to sun and wind. The fungal partner provides shade and protection from desiccation by sheltering the algae within its body. As a result, lichens are incredibly drought-resistant and can be found in a wide variety of habitats including some of the most extreme environments Earth has to offer. In fact the Rosette Lichen or Physica dubia grows in both Antarctica and the Mojave Desert!

Lichens are not just interesting from a biological perspective, but also a chemical one. Lots of lichens create and exude a suite of chemicals, the roles of which aren’t entirely known. Some are thought make the lichen distasteful to predators, while others may help block harmful UV rays and increase membrane permeability to facilitate the movement of nutrients, water, and cellular byproducts between algae and fungi.

These chemicals have also attracted the attention of scientists, as some exhibit antimicrobial, antiviral, anti-tumor, and insecticidal properties. Many are being analyzed and tested for a variety of medicinal and household uses and may soon become a key ingredient in a physician’s arsenal. Already, these organisms are utilized by humans in a number of different ways, and have been for hundreds of years.

In some native cultures around the globe, lichens are a part of the traditional diet for both people and livestock. However, most lichens have little nutritional value, are bitter tasting, and some can be toxic. Lichen extracts are also used as natural dyes for wool and cloth with colors ranging from browns and purples, to yellows and oranges. Other uses include the manufacture of perfume, cosmetics and sunscreen, a substitute for hops in brewing beer, and as a key ingredient in litmus paper.

Lichens are also sensitive to air pollution, and for that reason don’t typically grow too close to human habitation. In fact, lichens absorb pollutants into their tissues and for that reason can play an important role as an indicator species for pollution problems. As air pollution becomes more widespread, lichen species could be in danger of being lost. And because we have only scratched the surface of what these amazing organisms can do, who knows what future medicine could be lost along with it.

I could go on, as I have only scratched the surface of what these organisms can do. And in the coming years, I think we’ll hear of even more lichen-based breakthroughs in science and medicine. The next time you pass a colorful, lichen-covered rock, take a closer look at these incredible organisms and pause for a moment to wonder about the mysteries, and possible answers, that lie within.

For the Stokes Nature Center and Wild About Utah, this is Andrea Liberatore.

Credits:

Photos: Courtesy & © Andrea Liberatore
Text:    Andrea Liberatore, Stokes Nature Center, logannature.org

Additional Reading:

Ivins, Robert Fogel (1998) Lichens are Fungi! Utah State University Herbarium. Available online at: https://herbarium.usu.edu/fungi/funfacts/lichens.htm

Center for Ecological Sciences, Indian Institute of Science. Lichen Chemistry. Sahyadri E-news. Issue 34. Formerly available online at: https://wgbis.ces.iisc.ernet.in/biodiversity/sahyadri_enews/newsletter/issue34/lichens_chemistry/lichen_chemistry.pdf See https://www.researchgate.net/publication/257213745_Sahyadri_Shilapushpa_Lichen_Chemistry [Link updated Dec 1, 2023]

US Forest Service (2013) Celebrating Wildflowers: Lichens. Available online at: https://www.fs.fed.us/wildflowers/interesting/lichens/

 

Cicada Songs

Click for a larger view of a Crepitating Cicada. Courtesy and Copyright 2008 Jim Cane, Photographer
Crepitating Cicada
Platypedia putnami
Elko Co., Nevada
June 2008
Courtesy & Copyright 2008
Jim Cane, Photographer

Click for a larger view of a cast nymphal skin of a Crepitating Cicada. Courtesy and Copyright 2008 Jim Cane, PhotographerCast Nymphal Skin of the
Crepitating Cicada
Platypedia putnami
Elko Co., Nevada
June 2008
Courtesy & Copyright 2008
Jim Cane, Photographer

Click for a larger view of an Audiospectrograph of the Crepitating Cicada. Courtesy and Copyright 2008 Jim Cane, PhotographerAudiospectrograph of the
Crepitating Cicada
Platypedia putnami
Made with Raven Software
Elko Co., Nevada
June 2008
Courtesy
Jim Cane, creator

East Coast news reports have been abuzz about this summer’s synchronized emergence of the periodic cicada, last seen in 1996 when their parental generation flew. The incessant loud buzzing of these 17 year cicadas has been the dominant sound of mid-Atlantic forests and towns for some weeks now.

The Great Basin also has cicadas. Our two species from the genus Platypedia produce a more subdued mating call. They use crepitation, from the Latin for a crackling sound. Our crepitating cicadas have received scant research attention; even their means of sound production remains uncertain. Their call consists of a trill of accelerating clicks.

You can see an audio spectrograph of their clicking call on our Wild About Utah website. The wings of crepitating cicadas visibly clap to the tempo, leading some to believe that the sound is that of slapping wings. More likely, the snapping sound is generated by the bending of a wing vein or other semi-rigid surface in the manner of a metal dog training clicker. Listen to the similarity.

As with cicadas everywhere, our crepitating cicadas spend years underground as slow growing, wingless immatures called nymphs. Cicada nymphs feed in a manner similar to their smaller kin the aphids, white flies and scales, piercing the roots of trees and shrubs to suck their sweet sap. When and where adult cicadas are abundant, you can see scattered cast brittle skins from which the adults emerged. Tunneling by cicada nymphs has been shown to alter the morphology of Great Basin soils, but it is their collective daytime clicking that grabs your attention.

En masse, they sound like an orchestra of castanets. At sunset, as if on cue, they all become quiet for the night. After hearing our crepitating cicadas clicking all day long, that evening silence is profound.

Credits:

Images: Courtesy & Copyright 2008 Jim Cane, Photographer
Recording: Courtesy & Copyright Jim Cane
recorded with Raven software: Bioacoustics Research Program. (2011). Raven Pro: Interactive Sound Analysis Software (Version 1.4) [Computer software]. Ithaca, NY: The Cornell Lab of Ornithology. Available from https://www.birds.cornell.edu/raven.
Sound clip of the call of the 17-year periodic cicada, Courtesy Dan Mozgai, from his website, https://www.cicadamania.com/. Copyright Dan Mozgai.
Clicking sound of the crepitating cicada, Platypedia putnami. Logan Utah, June 2013. Copyright Jim Cane
Text: Jim Cane, https://bridgerlandaudubon.org/

Additional Reading:

Cicada Mania, https://www.cicadamania.com/