Category Archives: Mono Basin

Psathyrotes, Psathyrotopsis, and Trichoptilium (Oh, My!)

Recently I found myself looking closely at keys, descriptions, and photos of Psathyrotes annua (Annual turtleback) and P. ramosissima (“regular” Turtleback)—both rayless members of the Sunflower family, Asteraceae—to clear up some lingering uncertainty over how to distinguish the two. Then one taxon led to another and it became a larger project.

Psatyrotes annua is familiar to many who have wandered the perimeter of Mono Lake. It thrives in the sparsely vegetated sands and gravelly pumice of Mono’s prehistoric and post-1945 receding shorelines. It’s often misidentified as P. ramosissima, which so far, has probably not been found in the Mono Basin, but is common in the Mojave, Colorado, and western Sonoran Deserts. These two can be distinguished as follows:

  • Leaf blades generally clearly divided by deeply-set, anastomosing (cross-connecting) veins into irregular, ovate to polygonal areas (suggesting the segmented “scutes” of a turtle’s carapace); outer phyllaries ± wide, spatulate to obovate, widely spreading to reflexed; florets 21–26 (16–32) per head; pappus of 120–140 bristles in 3–4 series …… Psathyrotes ramosissima
  • Leaf blades generally weakly or not at all divided by veins into scute-like areas; outer phyllaries ± narrow, mostly lance-linear, ± erect to spreading; florets 13–16 (10–20) per head; pappus of 35–50 bristles in one series …… Psathyrotes annua
Psathyrotes ramosissima
Left: © Chloe & Trevor Van Loon/iNaturalist, Right: © Tom Chester/iNaturalist
Psathyrotes annua
Left: © Tim Messick/iNaturalist, Right: © Jim Morefield/iNaturalist

Exploring this small genus further, one finds there are currently three species in Psathyrotes, another close relative formerly in Psathyrotes now banished to Trichoptilium—a monotypic (one species) genus—and three more close relatives housed in Psathyrotopsis, a newer genus carved out of Psathyrotes.

Apparently no single key has been crafted that includes all 7 species of Psathyrotes, Trichoptilium, and Psathyrotopsis. The Jepson eFlora includes two Psathyrotes and the Trichoptilium. The Flora of North America (FNA) includes all three Psathyrotes, the Trichoptilium and one species of Psathyrotopsis, but not the other two, which appear to be narrow endemics in southern Coahuila, Mexico. Both Jepson and FNA make you work through ponderous keys for the entire sunflower family to distinguish these three genera. A paper on “Taxonomy of Psathyrotes” (Strother and Pilz 1975) includes a key to all of the taxa included in FNA, but not the third Psathyrotopsis, because it was described later (Turner 1993).

So, why not write a straightforward key that includes all seven taxa? Not so simple, it turns out, because existing keys don’t all use the same set of characters, and that newest species endemic to southern Coahuila (Psathyrotopsis hintoniorum) has never been included in a key with its relatives—and the paper describing it refers the reader to the formal description in Latin to figure out what distinguishes it from Psathyrotopsis purpusii. Thank goodness for Google Translate!

Below is an image of my key. (The very limited text formatting abilities in this WordPress blog don’t lend themselves to an indented key longer than 1 or 2 couplets.) The key is adapted from Baldwin 2012, Strother 2006a, Strother 2006b, Strother and Pilz 1975, and Turner 1973 (citations below). It has been modified from the originals by adding species, changing some terminology, rearranging some couplets, and adding some character states.

Here are photos of the rest of the species in Psathyrotes, Psathyrotopsis, and Trichoptilium (thank you to the iNaturalist contributors who allow their images to be used non-commercially!)

Psathyrotes pilifera Both: © slothiker/iNaturalist
Psathyrotyopsis hintoniorum
Left: © Arizona State University, Right: © New York Botanical Garden
(both are duplicate sheets of Guy Nesom 7648)
Psathyrotopsis purpusii Both: © José G. Flores Ventura/iNaturalist
Psathyrotopsis scaposa
Left: © Matt Reala/iNaturalist, Right: © Joey Santore/iNaturalist
Trichoptilium incisum
Left: © Jessica Irwin/iNaturalist, Right: © Irene/iNaturalist

And here are maps showing the known distribution of each species, produced (by me) using QGIS and Adobe Illustrator, based on occurrence data (the dots) from specimen locations served by the SEINet Portal Network and “Research Grade” observations from iNaturalist (note: some dots could be mismapped or misidentifications). Colored shading shows the approximate generalized distribution of each taxon.

References:
Baldwin, Bruce G. 2012. adapted from Strother (2006), Psathyrotes, in Jepson Flora Project (eds.) Jepson eFlora, https://ucjeps.berkeley.edu/eflora/eflora_display.php?tid=571, accessed on November 28, 2022.
Strother, John L., 2006a. Psathyrotes in Flora of North America 21:416–418 (http://www.efloras.org/florataxon.aspx?flora_id=1&taxon_id=126897), accessed on November 28, 2022
Strother, John L., 2006b. Psathyrotopsis in Flora of North America 21:364–365 (http://www.efloras.org/florataxon.aspx?flora_id=1&taxon_id=126898), accessed on November 28, 2022.
Strother, John L and George Pilz. 1975. “TAXONOMY OF PSATHYROTES (COMPOSITAE: SENECIONEAE).” Madroño; a West American journal of botany 23, 24–40. https://www.biodiversitylibrary.org/partpdf/169365
Turner, B. L. 1993. “A new species of Psathyrotopsis (Asteraceae, Helenieae) from Coahuila, México.” Phytologia 75, 143–146. https://doi.org/10.5962/bhl.part.17305.


Copyright © Tim Messick 2024. All rights reserved.

California Biodiversity Day Bioblitz for Mono

Users of iNaturalist in or near the Mono Basin might like to join (and thereby automatically contribute to) the “California Biodiversity Day 2020” Bioblitz for the greater Mono Lake area, including Lee Vining Canyon and Lundy Canyon. The project actually runs for a week, September 5 through 13, 2020. Details are on iNaturalist HERE.

I may not get over to Mono myself during this period, but I’ll be helping to identify observations that others make. Here’s a map showing the area in which observations will be added to the project (orange shading):

Map of the project area

Keep cool and hydrated out there — it’s going to be hot and a bit smoky the next few days.


UPDATE 9/6/2020: Oh well, never mind. Too much smoke from the Creek Fire in Fresno and Madera counties (https://inciweb.nwcg.gov/incident/7147/). Air quality is “hazardous” in Lee Vining, with the index over 350. (Up to 460 in Mammoth!) Shelter from the smoke!

Lee Vining WebCam on Sunday morning

Lee Vining WebCam on Sunday morning (https://www.monolake.org/today/lvcam)


Copyright © Tim Messick 2020. All rights reserved.
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Strolling around Panum Crater

Panum Crater in Google Earth

Panum Crater (foreground) and Mono Craters as seen in
Google Earth, looking southeast.

Panum Crater

One frosty morning in late October I walked around the narrow rim of Panum Crater, just south of Mono Lake. This is the youngest volcanic feature in the Mono Basin, so if you love landscapes built by fire and carved by ice, I highly recommend this hike, but do it in cool weather or very early on a summer day.

Panum Crater

Panum Crater

Panum Crater is only about 670 ±20 years old (circa 1320s to 1360s AD) (Sieh and Bursik 1986). The initial eruption was of the “Plinian” type, where abundant gases escape from the rising magma, producing a massive plume and rain of volcanic ash that may continue for weeks. (This is the same type of eruption that occurred on a larger scale at Italy’s Mt. Vesuvius in 79 AD, burying Pompeii and Herculaneum—witnessed and later described by Pliny the Younger, hence the name “Plinian.”) After the plumes of gas and ash subsided, magma welled up within Panum Crater to form a jagged dome of obsidian and pumice. Some time after the Panum Crater event, more ash fell throughout the area from eruptions several miles farther south in the Inyo Craters area.

Panum Crater

What would it have been like to see, hear, and smell this eruption, to feel the earth shake before and during the eruption? There were certainly Native Americans living here at that time — in the Mono Basin, the Bodie Hills, Bridgeport and Adobe Valleys, and on down to Owens Valley. We don’t know what time of year the eruption occurred, but there could have been groups traveling over Mono Pass and along other routes to trade with neighboring tribes when the eruption began.

Panum Crater

Laylander (1998) speculated on how earlier (ca. 880 AD) and larger Plinian eruptions in the Mono Craters may have affected local witnesses: “Local consequences for human populations from the eruption can be imagined. The event may have directly caused some loss of life or frightened the surviving witnesses into leaving the Mono Basin. The decimation of plant and animal communities may have drastically reduced the resource value of the affected area for humans for some time.” (He goes on to consider whether “an occupational hiatus, followed by a return to pre-event conditions” could be detected in the archaeological record and whether the duration of this hiatus could be estimated archaeologically. He concludes that “a hiatus of as much as a century is not likely to be detectable in the archaeological record” using hydration dating of artifacts, unless the sample size is “very large.”)

Panum Crater

Panum Crater

Banded obsidian and pumice atop the dome.

Panum Crater

Panum Crater

Panum Crater

Panum Crater is not quite the youngest cinder cone in California — that distinction may belong to Cinder Cone in Lassen Volcanic National Park, which erupted about 300 years later, circa 1650. And Lassen Peak itself erupted last in 1915.

References:
Laylander, D. 1998, Cultural Hiatus and Chronological Resolution: Simulating the Mono Craters Eruption of ca. A.D. 880 in the Archaeological Record, Proceedings of the Society for California Archaeology 11:148-154.

Sieh, K. and M. Bursik 1986. Most recent eruption of the Mono Craters, eastern central California. Journal of Geophysical Research, 91(B12): 12,539–12,571.


Copyright © Tim Messick 2020. All rights reserved.
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