Cicindela decemnotata

Say, 1817

Badlands Tiger Beetle

Cicindela decemnotata, commonly known as the badlands , is a flashy tiger beetle in the . It is the westernmost representative of a species group characterized by green coloration with variable red markings on the , , and . The species has undergone recent and rapid phylogenetic radiation following glacial recession, with five recognized based on morphological and molecular evidence. show relatively low genetic divergence despite marked morphological differences, suggesting within the past 10,000 years.

Cicindela decemnotata meriwetheri by no rights reserved, uploaded by Ben Keen. Used under a CC0 license.Cicindela decemnotata decemnotata by (c) Kathy Lichtendahl, some rights reserved (CC BY), uploaded by Kathy Lichtendahl. Used under a CC-BY license.American entomology (Plate 18) (6026026255) by Say, Thomas. Used under a Public domain license.

Pronunciation

How to pronounce Cicindela decemnotata: //sɪˈsɪndələ dɛˌsɛmnoʊˈtɑːtə//

These audio files are automatically generated. While they are not always 100% accurate, they are a good starting point.

Identification

Distinguished from related by the sharply angled elytral that does not reach the elytral edge, combined with green and variable red coloration. Most similar to Cicindela limbalis, C. splendida, and C. denverensis, which occur further east in the Great Plains, and to C. sexguttata, C. patruela, and C. denikei in forested regions to the east. The 'greasy' appearance and specific maculation pattern separate it from these relatives. Five (C. d. albertina, C. d. bonnevillensis, C. d. decemnotata, C. d. meriwetheri, C. d. montevolans) are recognized based on geographic distribution and subtle morphological differences.

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Habitat

Inhabits alkaline flats, sandy ridges, and open sagebrush landscapes in arid western regions. Often found on exposed sandy soils rather than the most obvious alkaline flat surfaces. Associated with badlands topography and post-glacial landscapes in the northern Great Plains, northern Great Basin, and Rocky Mountain regions.

Distribution

North America: Rocky Mountains from northwestern Great Plains and northern Great Basin north to Yukon. Easternmost records from northwestern Nebraska; occurs more reliably in Wyoming and westward. Distribution largely confined to areas uncovered by glacial ice within the last 10,000 years.

Seasonality

active in late summer and fall; observations from September and October documented. Activity likely limited by cooler temperatures at northern latitudes and higher elevations.

Life Cycle

Larval stage has been observed in suitable sandy ; details of development and otherwise poorly documented.

Behavior

are fast-running and can be skittish, though some individuals tolerate close approach. Exhibits thermoregulatory behaviors including stilting when active in open, sunny . Readily takes when disturbed after initial escape running.

Ecological Role

Predatory occupying open, arid ; likely functions as an in sandy and alkaline flat . Part of a post-glacial colonizing fauna with rapid recent radiation.

Human Relevance

Subject of entomological and photography, particularly sought after by enthusiasts due to its restricted distribution and distinctive appearance. Five described in 2012 based on combined morphological and molecular study, contributing to understanding of rapid post-glacial speciation.

Similar Taxa

  • Cicindela limbalisOccurs further east in Great Plains; part of same but with different geographic range and maculation details
  • Cicindela splendidaEastern Great Plains relative with similar green-red coloration but distinct distribution and subtle morphological differences
  • Cicindela denverensisPartially member occurring further east
  • Cicindela sexguttataMore eastern, forested with related but different ecological preferences
  • Cicindela patruelaEastern forest-dwelling relative in same group
  • Cicindela denikeiEastern forest with related ancestry but distinct and distribution

More Details

Subspecies and Recent Radiation

Molecular and morphological analyses support recognition of five : C. d. decemnotata (nominate), C. d. albertina, C. d. bonnevillensis, C. d. meriwetheri, and C. d. montevolans. Three subspecies were described as new in 2012 by Knisley, Woodcock, and Kippenhan. Low genetic divergence combined with marked morphological differences indicates rapid phylogenetic radiation following glacial recession within the last 10,000 years, paralleling patterns seen in the Cicindela maritima group.

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Sources and further reading