Red leaves in autumn: What’s in it for the tree?

Red leaves in autumn: What’s in it for the tree?: Canyon or Big-Toothed Maple leaves in late summer, Acer grandidentatum, Courtesy Michael Kuhns, https://Extension.usu.edu/treebrowser/
Searsh Extension.usu.edu/treebrowser/ for Canyon or Big-Toothed Maple
leaves in late summer
Acer grandidentatum
Courtesy Michael Kuhns

Canyon or Big-Toothed Maple leaves in fall, Acer grandidentatum, Courtesy Michael Kuhns, Extension.usu.eduCanyon or Big-Toothed Maple
leaves in fall
Acer grandidentatum
Courtesy Michael Kuhns

Hi, I’m Holly Strand.

As early as 4th grade, children learn that leaves are green because of the high concentration of chlorophyll relative to other pigments. And that autumn leaves turn color because the breakdown of chorophyll molecules unmasks the yellow, orange and red pigments that remain.

This simple and satisfying explanation has existed for awhile. However, research in the past 15 years has uncovered a much more complicated story. Leaf physiologists jumped from the question, “What makes autumn leaves so colorful?” And started to ask the evolutionary question: “What’s the purpose behind this autumn color fest?” “What’s in it for the tree itself?”

The group of pigments that produce yellow or orange are called carotenoids. The carotenoids are in the leaf throughout the growing season but only become apparent with the breakdown of chlorophyll into colorless metabolites. However, the red pigments—or anthocyanins– are produced in the leaf AFTER much of the chlorophyll is lost. This active production of new anthocyanins led scientists to believe that the pigment must be performing a critical function.

Just what function is still not known but many hypotheses exist. One is that anthocyanins act as a sunscreen shielding leaf tissues against the harmful effects of sunlight. The risk of sun damage is particularly high in fall because of the lack of chlorophyll protection and because there is increased light due to a thinning canopy. Without sun damage, the leaves can continue to absorb nutrients right up to the end.

Another possibility is that anthocyanins function as an antioxidant shield. Plant chloroplasts produce fewer free radicals when shielded from green wavelengths of light. Anthocyanins absorb the green wavelengths. Without anthocyanin, a surplus of superoxides could cause damage to the plant cell structure.

Lastly, there is the coevolution hypotheses. Aphids and other insects feed, carry viruses and bacteria. So red coloration was an adaptation developed by trees designed to lighten their insect load. The red leaves signal to insects that the tree is not a suitable host. The coevolution theory is supported in part because trees with autumn colors tend to be the ones with a history of interaction with aphids. Also, experiments have shown that most aphids strongly prefer green leaves over red leaves. In some cases anthocyanin may be positively correlated with a form of chemical defense.

However, when considering this last theory, remember that species perceive color differently. To the human eye, a tree may be a brilliant autumn shade of red. To the aphid, that same tree might be an indistinguishable gray. Further the insect may be avoiding red leaves because of differences in texture, taste, scent, texture or something else that is important to an aphid.

Whatever the reason is, I hope you are enjoying Utah’s colorful reds and yellows.

For links to current research and a Forest Service update on fall color around the state, go to www.wildaboututah.org.

For Wild About Utah, I’m Holly Strand.

Credits:


Images: Courtesy and Copyright 2003 Michael Kuhns, Extension.usu.edu
Text: Holly Strand

Sources & Additional Reading


USDA Forest Service Fall Colors web site for the Intermountain Region https://www.fs.usda.gov/detail/r4/recreation/?cid=FSBDEV3_016189

Archetti, M., Doring, T. F., Hagen, S. B., Hughes, N. M., Leather, S.
R., Lee, D. W., Lev-Yadun, S., Manetas, Y., Ougham, H. J., Schaberg,
P. G., Thomas, Howard (2009). Unravelling the evolution of autumn
colours: an interdisciplinary approach. Trends in Ecology and
Evolution, 24, (3), 166-173. https://digitalcommons.fiu.edu/cas_bio/38/
[FIU moved to behind a paywall-URL updated 260111-https://fiu-flvc.primo.exlibrisgroup.com/discovery/fulldisplay?docid=cdi_proquest_miscellaneous_66985692&context=PC&vid=01FALSC_FIU:FIU&lang=en&search_scope=MyInst_and_CI&adaptor=Primo%20Central&tab=All40&query=any,contains,Unravelling%20the%20evolution%20of%20autumn%20colours:]

Chittka L, Döring TF (2007) Are Autumn Foliage Colors Red Signals to
Aphids? PLoS Biol 5(8): 187. https://journals.plos.org/plosbiology/article?id=10.1371/journal.pbio.0050187

Lee, David and Kevin S. Gould Why Leaves Turn Red. American
Scientist, Volume 90. 524-531 https://harvardforest.fas.harvard.edu/sites/harvardforest.fas.harvard.edu/files/leaves/2002_11_leaf_article.pdf

Gunnell, JayDee, Reese, Julene, Ask a Specialist: What Causes the Fall Leaves to Change Color?, USU Cooperative Extension, https://extension.usu.edu/htm/news-multimedia/articleID=18662

Aflame with Color

Aflame with Color: Canyon or Big-Toothed Maple In a natural landscape Acer grandidentatum, Courtesy Michael Kuhns Extension.usu.edu
Canyon or Big-Toothed Maple
In a natural landscape
Acer grandidentatum
Courtesy Michael Kuhns
Extension.usu.edu

Holly: Hi, I’m Holly Strand from Stokes Nature Center in beautiful Logan Canyon.

The canyons and valleys of Utah will soon be awash with brilliant fall hues. Cascades of red, orange and gold will blanket the hillsides as the weather turns cooler and morning frost dusts the mountain ridges.

The Canyon Maple is one of Utah’s main sources of autumn color. Like most maple species, its leaves are carved into deep lobes. The leaves are medium-to-bright green now, but soon the entire tree will glow with spectacular color.
Canyon maple is found throughout Utah at medium elevations between 4,500 to 7,500 feet. It tends to grow on lower slopes and canyon bottoms in the mountains in association with Douglas-fir and junipers.

Its scientific name, Acer grandidentatum [AY-ser gran-dih-den-TAY-tum], means “Big Tooth”, referring to the tree’s distinctive lobed leaves with large, toothed margins. In fact, bigtooth maple is another common name for this species.

Canyon or Big-Toothed Maple In a natural landscape Acer grandidentatum  Courtesy Michael Kuhns Extension.usu.edu
Canyon or Big-Toothed Maple
In a natural landscape
Acer grandidentatum
Courtesy Michael Kuhns
Extension.usu.edu

Some think that he canyon maple is related to the sugar maple of the northeastern and midwestern United States,” says forestry professor Mike Kuhns of Utah State University’s Department of Wildland Resources. It’s possible that long ago, the Rocky Mountains rose up and isolated a sugar maple population that eventually evolved into a unique species.

The canyon maple rivals its eastern relatives in fall color but does it produce sap suitable for tasty, syrup-covered waffles and pancakes? Back in 1970s, a group of scientists set out to determine just that. The trees were tapped and yielded plenty of sticky liquid. The color was very light, resembling light honey and the flavor was delicate and fruity, almost like pineapple. However, it was notably less sweet than the northeastern sugar maple. Of 30 panelists from Utah who participated in a taste test, 57 percent preferred eastern sugar maple syrup but the remaining 43 percent preferred canyon maple syrup.

Canyon or Big-Toothed Maple leaves in late summer Acer grandidentatum Courtesy Michael Kuhns
Canyon or Big-Toothed Maple
leaves in late summer
Acer grandidentatum
Courtesy Michael Kuhns

The researchers concluded that while canyon maple sap was not practical for large-scale syrup production it might be enjoyable for individuals to try on a small scale on private land within its habitat range.

Syrup aside, the medium-sized tree thrives in Utah’s residential landscapes, parks and urban areas, as well as in the wild. Its year-round beauty, hardiness and manageable size make it a perennial favorite in the Beehive State.

Thanks to the USU College of Natural Resources for supporting research and development of this Wild About Utah topic.

For Wild About Utah and Stokes Nature Center, I’m Holly Strand.
Credits:

Canyon or Big-Toothed Maple leaves in late summer & fall Acer grandidentatum  Courtesy Michael Kuhns Extension.usu.edu
Canyon or Big-Toothed Maple
leaves in late summer & fall
Acer grandidentatum
Courtesy Michael Kuhns
Extension.usu.edu

Image: Courtesy and Copyright 2003 Michael Kuhns, Extension.usu.edu

Text: Holly Strand & Mary-Ann Muffoletto, Stokes Nature Center

Sources & Additional Reading:

 

Barker, Phillip A.; Salunkhe, D. K. 1974. Maple syrup from bigtooth maple. Journal of Forestry. 72(8): 491-492. [9065] https://www.ingentaconnect.com/content/saf/jof/1974/00000072/00000008/art00016

Kuhns, Michael. 2003. Canyon Maple: A Tree For the Interior West,” USU Forestry Extension, https://extension.usu.edu/forestry/HomeTown/Select_CanyonMaple.htm [2009, September 16].

Tollefson, Jennifer E. 2006. Acer grandidentatum. In: Fire Effects Information System, [Online]. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory (Producer). Available: https://www.fs.fed.us/database/feis/ [2009, September 16]

Acer grandidentatum – Bigtooth Maple, Water-wise Plants for Utah Landscapes, https://www.waterwiseplants.utah.gov/default.asp?p=PlantInfo&Plant=17

Colorado Pikeminnow

Colorado Pikeminnow, Image courtesy US FWS, J.E. Johnson, Photographer

Colorado Pikeminnow
Ptychocheilus lucius
Image courtesy US FWS,
J.E. Johnson, Photographer

One of the largest minnows in the world, the Colorado pikeminnow was once found throughout the Colorado River basin. This is no bait minnow. Also known as the Colorado squawfish, it reputedly grew to a whopping 6 feet in length with a weight topping 80 pounds and a life span of 40 years. The largest caught in recent times have been only 3 feet long and 9 pounds.

Colorado pikeminnows once flourished throughout the Colorado River and most of its major tributaries. Historically, these abundant, torpedo-shaped fish were prized for their fine flavor. They were an important food fish for Native Americans and welcomed at restaurants as far away as San Francisco. Also called white salmon by early settlers due to their migratory behavior, pikeminnows journeyed 200 miles to spawn in turbid backwaters.

Then we built dams which blocked the migratory runs of pikeminnows. Below the Grand Canyon, the last wild Colorado pikeminnow was caught in 1976. The proliferation of dams has drastically restricted their range. Moreover, reservoirs flood what was suitable river habitat, and their dams alter river flows and water temperature downstream.

The Colorado pikeminnow was one of the first fish given full protection under the Endangered Species Act in 1973. Today, there are two remaining wild populations. One resides in the upper reaches of the Colorado river system, the other in the Green River system. Efforts underway to restock Colorado pikeminnow in the San Juan River basin appear to be successful.

A broadly based coalition of partners established the Upper Colorado River Endangered Fish Recovery Program in 1988. This program focuses on 4 species of fish: humpback chub, bonytail, Colorado pikeminnow and razorback sucker. Their goal is to restore and manage stream flows and habitat, reduce competition from some non-native fish species and increase populations using hatchery raised young. If they are successful, this giant piscine predator will once again take its rightful place in the upper Colorado River ecosystem.

This is Linda Kervin for Bridgerland Audubon Society.

Credits:

Photos: Courtesy US FWS, images.fws.gov
Theme: Courtesy & Copyright Don Anderson Leaping Lulu
Text & Voice: Linda Kervin, Bridgerland Audubon Society

Additional Reading:

Other Wild About Utah Pieces by Linda Kervin

Colorado Pikeminnow, Wikipedia, wikipedia.org/wiki/Colorado_pikeminnow

Researchers Capture Fourth Largest Endangered Colorado Pikeminnow in San Juan River Since 1991, US Fish & Wildlife Service, December 13, 2010, https://www.fws.gov/mountain-prairie/pressrel/10-84.htm [Link Updated December 2023]

Colorado pikeminnow (Ptychocheilus lucius), Upper Colorado River Endangered Fish Recovery Program, 2012, https://www.coloradoriverrecovery.org/general-information/the-fish/colorado-pikeminnow.html [Link Updated December 2023]

Colorado Pikeminnow, Nevada Department of Wildlife, Formerly held at https://www.ndow.org:80/wild/animals/facts/fish_colorado_pike_minnow.shtm [Not working December 4, 2023]

Colorado Pikeminnow, Species, Utah Division of Wildlife Resources, https://fieldguide.wildlife.utah.gov/?species=ptychocheilus%20lucius [Link Updated December 2023]

https://wildlife.state.co.us/Fishing/SpeciesID/Pages/FishID.aspx [Not working December 4, 2023]

https://wildlife.utah.gov/fishing/nonnative/endangeredfishfacts.pdf [Not working December 4, 2023]

Colorado Pikeminnow endangered in Carbon, Daggett, Emery, Garfield, Grand, San Juan, Unitah and Wayne Counties, Utah’s Species of Greatest Conservation Need Species by County,
https://wildlife.utah.gov/pdf/WAP/utah-sgcn-list-by%20county-10-23.pdf

Utah’s Glacial History

Moraine with erratics, Photo Courtesy and Copyright Mark Larese-Casanova, Photographer
Moraine with erratics
Photo Courtesy & Copyright
Mark Larese-Casanova, Photographer

Little Cottonwood Canyon, Photo Courtesy and Copyright Mark Larese-Casanova, PhotographerLittle Cottonwood Canyon
Photo Courtesy & Copyright
Mark Larese-Casanova, Photographer

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

It is amazing to see just how much of an impact the large amount of snowfall from last winter still has on the annual cycle of nature. Of recent note, wildflower blooms in the mountains seem to be at least 2-3 weeks behind normal schedule. Hiking through snow in late July had me thinking about colder times when Utah’s mountains were covered with ice that flowed as glaciers.

The most recent period of glaciation in Utah occurred between 30,000 and 15,000 years ago when Utah’s climate was, on average, up to 30?F cooler. At times during this period, much of the western half of Utah was covered by Lake Bonneville, which contributed tremendous amounts of moisture as snow throughout Utah’s mountain ranges. As the snow accumulated at high elevations, its sheer weight caused it to recrystallize into ice. Once the masses of ice became heavy enough, gravity pulled them down slope, carving out characteristic U-shaped valleys.

At the top of the valleys, where the glaciers formed, we can often find large, bowl-shaped cirques. In the Wasatch Range, the Little Cottonwood Canyon glacier formed at the top, creating Albion Basin, and reached the mouth of the canyon where calved icebergs into Lake Bonneville. The Uinta Mountains contained such large glaciers that even many of the mountain peaks are rounded.

As temperatures warmed during the end of the last ice age, glaciers receded and left behind large piles of soil and rocks, known as moraines. Terminal moraines at the end of a glacier’s path, can act as natural dams to create lakes. Enormous boulders, known as glacial erratics, can often be found discarded along canyons.

While glaciers don’t currently exist in Utah, there are several permanent snowfields in shaded high mountain areas. So, if you’re feeling a little nostalgic and missing that extra long winter we had this year, you still a chance to hike up above 9,000 feet and cool your toes in the snow.

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

Credits:

Images: Courtesy & 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/surveynotes/gladasked/gladglaciers.htm

Parry, William T. 2005. A Hiking Guide to the Geology of the Wasatch and Uinta Mountains. University of Utah Press.

Stokes, William Lee. 1986. Geology of Utah. Utah Museum of Natural History.