Research Article |
Corresponding author: Luis Espinasa ( luis.espinasa@marist.edu ) Academic editor: Ľubomír Kováč
© 2024 Luis Espinasa, Abrianna Gutierrez, Amata Hinkle, Matthew L. Niemiller.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Espinasa L, Gutierrez A, Hinkle A, Niemiller ML (2024) A new genus and species of nicoletiid silverfish (Insecta, Zygentoma, Nicoletiidae) from caves of northern Alabama, USA. Subterranean Biology 49: 1-17. https://doi.org/10.3897/subtbiol.49.119986
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A new genus and species of troglobiotic nicoletiid (Insecta, Zygentoma, Nicoletiidae) is described from northern Alabama, USA. The type species was collected from three caves in the Highland Rim section of the Interior Low Plateau physiographic province on the northern side of the Tennessee River Valley. Morphological and genetic analysis using the mitochondrial 16S rRNA locus show that Spinanycta alabamensis sp. nov. is quite distinct from related nicoletiids in North America. The species differs from members of other genera by its urosternum I, which in males is modified with a central pointy extension. The new species significantly extends the distribution of cave-dwelling members of the family into the southeastern United States and suggests that additional nicoletiid diversity remains to be discovered from karst regions of the eastern United States.
Insect, Interior Low Plateau, subterranean, Thysanura, troglobite, troglobiont
Among the insects, Silverfish (order Zygentoma) are some of the most intriguing. This group diverged before the appearance of wings and thus are considered among the earliest, most primitive insects. Their predecessors were among the first arthropods to colonize terrestrial habitats and were present during the Silurian Period more than 400 million years ago (
Distribution of cave-dwelling nicoletiid genera in northern Mexico and the southern United States. Shaded areas are municipalities and counties in Mexico and the United States, respectively, with documented occurrences for each genus. Dark gray shaded areas are karst exposures in the United States. Inset is the distribution of Spinanycta alabamensis sp. nov. in northern Alabama with Alabama Cave Survey cave codes labeled. Bobcat Cave (AMD1283) is the type locality.
Here we describe a new genus and species of cave nicoletiid from caves of the Interior Low Plateau karst region in northern Alabama, recently discovered during cave biosurveys in the region. The new species significantly extends the distribution of cave-dwelling members of the family into the southeastern United States and increases the likelihood that additional diversity remains to be discovered in the Interior Low Plateau and other karst regions of eastern North America.
Specimens were collected as part of a biological inventory of cave life in northern Alabama. Biosurveys consisted of visual encounter surveys (VESs) by a minimum of two people for at least two-person hours in all caves. VESs of terrestrial habitats included the cave floor, walls, and ceiling, as well as underneath rocks, logs, and other debris when available. Any cover objects were returned to their original positions to minimize microhabitat disturbance. Specimens encountered were collected by hand and preserved in 100% ethanol, then stored at -20 °C for molecular analysis. Specimens were accessioned into the Entomology Collection at the Auburn Museum of Natural History.
Specimens were examined and dissected using a Motic stereomicroscope. Photographs of some structures were recorded using an iPhone 12 mini camera attached to the dissecting microscope. Photographs were taken in multiple focal planes and processed so that the whole image was in focus using the Zerene Stacker software package (Zerene Systems LLC, Richland, Washington, USA). Drawings of some pertinent structures were prepared with the aid of camera lucida attached to a Motic dissecting microscope.
Genomic DNA was extracted using Qiagen’s DNEasy® Tissue Kit by digesting a leg in lysis buffer from five specimens from Muddy Cave in Madison County, Alabama (Alabama Cave Survey (ACS) cave no. AMD1095) collected on 7 July 2022, one from Rockhouse Cave in Limestone County, Alabama (ACS no. ALM312) collected on 21 May 2020, and the holotype and three paratypes from Bobcat Cave in Madison County, Alabama (ACS no. AMD1283) collected on 26 November 2019.
PCR amplification and Sanger sequencing of a portion of the mitochondrial 16S rRNA locus followed standard protocols and primers (16Sar and 16Sb) used in the past for nicoletiids (
BLAST analysis was done to determine the most similar sequences in GenBank. Sequences of all other nicoletiid species available were aligned and a preliminary tree analysis was performed in ClustalW2 (ML tree was inferred using PhyML v20160115 ran with model and parameters: -o tlr -f m --pinv e --bootstrap -2 --alpha e --nclasses 4. Branch supports are the Chi2-based parametric values return by the approximate likelihood ratio test). DNA sequences for specimens are in NCBI’s GenBank (accession no. PP057689).
We conducted both NatureServe and IUCN Red List conservation assessments for the newly described species. For the IUCN Red List assessment, the risk category was calculated using RAMAS Red List 3.0 (
Order Zygentoma Börner, 1904
Suborder Neozygentoma Engel, 2006
Infraorder Euzygentoma Grimaldi & Engel, 2005
Family Nicoletiidae Escherich, 1905
An American nicoletiid with Urosterna II–VII subdivided into two coxites and one sternite. Urosterna I, VIII and IX of male entire. Coxites on segments II–IX with styli. Urosternum I of males modified with a central pointy extension. Urosternum VIII of male flat posteriorly, without emarginations or projections in between the styli of this segment. Paramera with a distal semi-eversible vesicle and short chaetae, their length being about 1/4 the width of the paramera. Subgenital plate of females subtriangular. Tergum X with one distinct macrochaetae on posterior angles. Cercus of male with sensory pegs (spines) and appendix dorsalis without sensory pegs.
Pedicellus of adult male with unicellular glands. Mouthparts not specialized. Mandible strongly sclerotized apically with usual teeth. Apex of galea with two conules; one longer than wide and the other wider than long. Lacinia heavily sclerotized distally. First process of lacinia pectinate. Labium without prominent lateral lobes.
Tarsi with four articles. Praetarsi with three simple claws. Median claw glabrous, slender and smaller than lateral claws. Urosterna II–VII subdivided into two coxites and one sternite. Urosterna VIII and IX of male entire. Median portion of sternites with 1+1 sublateral macrochaetae at hind borders, as well as 1+1 macrochoetae near suture at about middle of segment. Coxites on segments II–IX with styli. Eversible vesicles on segments II–VI, pseudovesicles on VII. Urosterna I of males modified with a central pointy extension. Urosterna III and IV of adult males apparently without modifications. Urosternum VIII of male straight posteriorly, without emarginations or projections in between the styli of this segment. Tergum X with 1+1 distinct macrochaetae on posterior angles.
Point of insertion of paramera apparently slightly deep. Paramera with a distal semi-eversible vesicle, but less prominent than in Texoreddellia (
Sequences generated for the mitochondrial 16S rRNA locus for all ten specimens from the three different caves were 529 bp long and identical. BLAST analysis showed this 16S haplotype to be quite different from any sequence available in GenBank (maximum of 77.26 Per. ident.). Within the American Nicoletiidae, Spinanycta differs from the genus Allonicoletia Mendes, 1992 by 130 bp (24.5%), from Speleonycta by 132 bp (24.9%), from Texoreddellia by 134 bp (25.3%), from Squamigera Espinasa, 1999 by 138 (26.0%), from Gibboletia Espinasa & Smith, 2023 by 145 bp (27.4%), from Prosthecina by 148 bp (27.9%), from Anelpistina by 155 (29.3%), and from Nicoletia Gervais, 1843 by 153 bp (28.9%). Using the 16S rRNA fragment sequences of nicoletiid species across the subfamily Cubacubaninae (
Maximum-likelihood phylogenetic analysis showed that members of genera Speleonycta, Allonicoletia, Texoreddellia and Nicoletia form a well-supported clade, with the Alabama specimens as sister to this group, and also in a clade distinct from other nicoletiid genera including Anelpistina. These results indicate that the Alabama nicoletiids belong to a group independent from any previously described genera for which 16S rRNA sequences are available. Acanthonima Espinasa, 2005 has yet to have its DNA sequenced, but morphologically it is very different from the Alabama specimens (See below). Resolving the placement of all aforementioned genera within subfamilies was beyond the goals of the current study.
Spinanycta alabamensis sp. nov.
Spinanycta. From spina = Greek for spine. It references the diagnostic spine in urosterum I, and nycta = Greek for night. It references in Greek mythology the occupation of caves by Nyx, the primordial goddess of night.
Spinanycta alabamensis belongs to the American Nicoletiidae characterized by subdivided abdominal sterna II–VII and fused coxites of abdominal segments VIII and IX (Cubacubaninae + Nicoletiinae;
The type species of the new genus shares some characteristics with Speleonycta, Allonicoletia, Texoreddellia, and Nicoletia, such as the paramera with semi-eversible vesicles, urosternum VIII of male straight posteriorly without emarginations or projections in between the styli of this segment. None of these characteristics are present in any of the other genera of Cubacubaninae. The new genus can easily be distinguished from Speleonycta because it lacks the very long and specialized chaetae in the distal semi-eversible vesicle of the paramera. From Allonicoletia they can further be differentiated by the presence of styli on urosternite II. From Texoreddellia and Squamigera by the absence of scales. From Prosthecina by the absence of conspicuous lateral lobes bearing numerous glandular pores in the submentum. From Anelpistina as defined by
This genus is known from just three cave systems on the north side of the Tennessee River Valley in southern Madison and southeastern Limestone counties, Alabama, within the Highland Rim section of the Interior Low Plateau physiographic province (Fig.
Holotype : male 8.5 mm, from Bobcat Cave (34.6686°N, 86.7130°W), Alabama Cave Survey (ACS) no. AMD1283. Redstone Arsenal, Madison County, Alabama, USA, deposited into the Entomology Collection at the Auburn Museum of Natural History (AUM 221500), collected 26 November 2019 by Matthew L. Niemiller, Joseph Lamb, Amata Hinkle, and Brian Stoltz (field code MLN 19-050).
Paratypes : 3♀ paratypes with same collection information as holotype (AUM 221501–221503); 1♂, 3♀ paratypes from Bobcat Cave collected on 6 October 2020 by Matthew L. Niemiller, Joseph Lamb, and Amata Hinkle (field code MLN 20-036.6) (AUM 221504–221507); and 1♂, 1♀ from Bobcat Cave collected 13 September 2023 by Amata Hinkle, Brendan T. Cramphorn, Jared P. Higgs, and Eric C. Maxwell (field code BTC 23-019-1) (AUM 221508–221509).
Additional material : 2♂, 2♀ from Muddy Cave (ACS no. AMD1095), Madison County, Alabama, USA, collected 15 June 2020 by Matthew L. Niemiller, K. Denise Kendall Niemiller, Amata Hinkle, Joseph Lamb, and Katherine E. Dooley (field code MLN 2020-021.1) (AUM 221510–221513); 1♂, 2♀ from Muddy Cave collected 7 July 2022 by Matthew L. Niemiller, Brendan T. Cramphorn, and Eric Cline (field code BTC 22-110-3) (AUM 221514–221516).
1♀ from Rockhouse Cave (ACS no. ALM312), Wheeler National Wildlife Refuge, Limestone County, Alabama, USA collected 21 May 2020 by Matthew L. Niemiller, K. Denise Kendall Niemiller, Amata Hinkle, and Katherine E. Dooley (field code MLN 20-020.6) (AUM 221517).
S. alabamensis. Derived from the word Alabama, the state where the species was discovered.
USA. Alabama, Madison County, Bobcat Cave (ACS no. AMD1283) on Redstone Arsenal. Redstone Arsenal is a 154.8 km2 United States Army installation in southwestern Madison County adjacent to the city of Huntsville. Redstone Arsenal is host to more than 75 tenant agencies, including the Department of Defense, Department of Justice, Federal Bureau of Investigation, and, most notably, the National Aeronautics and Space Administration’s Marshall Space Flight Center. Bobcat Cave is located near the western border of Redstone Arsenal (34.6686°N, 86.7130°W) on a small knoll. Redstone Arsenal and Bobcat Cave are situated within the Tennessee River District of the Highland Rim section of the Interior Low Plateau Province. The cave is developed in the Tuscumbia Limestone with a mapped length of 454.1 m (1,490 ft) and vertical extent of 6.4 m (21 ft). Much of the cave consists of a series of low and broad passages connected by tight crawlways with little exposure of bedrock. Water levels in the cave respond quickly to heavy precipitation and can flood completely. Significant flooding events continually deposit mud on nearly all surfaces in the cave. It is on these mud substrates and under the few mud-encased rocks nearer the entrance that most Spinanycta alabamensis have been found. In addition, individuals have been observed on the surface of isolated pools in the Shrimp Room, the largest room in the cave (61 m by 30.5 m).
Male holotype 8.5 mm (Fig.
Spinanycta alabamensis sp. nov. A male holotype (left) and female paratype (right) B–L male holotype B, C pedicellus D head E macrochaetae by insertion of antennae F labium G last article of labial palp H sensilla of maxillary palp I maxilla J apex of lacinia K conules of galea L sensilla of maxillary palp.
Mouthparts as shown in Figs
Thorax as in Fig.
Posterior end of urotergite X with a 1+1 long macrochaetae (Fig.
Urosternum VIII of adult male flat between the insertion of the styli (Fig.
Spinanycta alabamensis sp. nov., A, B male paratype C–G female paratypes A male genital area B parameres highlighting (red arrow) distal semi-eversible vesicle C, D ovipositor E, F variability in the subtriangular shape of the subgenital plate G apex of subgenital plate highlighting (red arrow) its slight point.
In adult females, the ovipositor surpasses apex of stylus IX between 3 and 3+2/3 the length of the stylus IX (Fig.
Males at 5.5 mm have no glands in pedicellus, no spine in urosternum I, or spines in cerci, but they already have paramers. At 6.5 mm they have glands in the pedicellus, the spine in urosternum I reaches about ¾ of the apex of urosternum II, and spines in cerci are small. At 7 mm the spine reaches the apex of urosternum II and by 8.5 mm it surpasses by 1/10 the length urosternum II.
Females at 5.5 mm have an ovipositor that barely surpasses the apex of stylus IX and gonapophyses with about 15 divisions. By 7 mm ovipositor surpasses apex of stylus IX by about 2+2/3 the length of the stylus and the gonapophyses has the adult number of 21–22 divisions. Between 7.2 mm and 10.5 mm in the largest available specimen the ovipositor surpasses stylus IX by between 3 and 3+2/3 the length of the stylus.
The species is known to date only from three caves, all developed in the Tuscumbia Limestone and located along the northside of the Tennessee River in southern Madison and southeastern Limestone counties. The largest population at Bobcat Cave is located on Redstone Arsenal. Muddy Cave is owned and managed by the Land Trust of North Alabama and is located 15.1 km SE of Bobcat Cave adjacent to a large residential area. Rockhouse Cave is located 16.5 km SW of Bobcat Cave and is developed in an exposure of limestone, Rock House Bluffs, on the north shore of the Tennessee River on Wheeler National Wildlife Refuge. The current distribution represents an EOO of 124.1 km2 and AOO of 12.0 km2.
At Bobcat Cave, Spinanycta alabamensis has been observed actively crawling on mudbanks and underneath mud-covered cobble and rocks adjacent to pools in the dark zone below the slope from the entrance and throughout the Shrimp Room (Figs
Observations of Spinanycta alabamensis sp. nov. from the three known localities in northern Alabama, USA.
Date | No. observed | |
---|---|---|
Bobcat Cave (AMD1283), Madison Co., Alabama | 26 Nov 2019 | 7 |
6 Oct 2020 | 5 | |
13 Sep 2023 | 20 | |
Muddy Cave (AMD1095), Madison Co., Alabama | 15 Jun 2020 | 13 |
7 July 2022 | 4 | |
25 Sep 2022 | 1 | |
27 Aug 2023 | 0 | |
Rockhouse Cave (ALM312) Limestone Co., Alabama | 21 May 2020 | 1 |
24 Nov 2021 | 0 | |
3 April 2022 | 0 |
Spinanycta alabamensis is known currently from three caves in southern Madison and southeastern Limestone counties, Alabama. The species was assessed as Imperiled (G2) under NatureServe criteria and as Endangered B1a under IUCN Red List criteria because of few known occurrences, a small and potentially restricted geographic range, high intrinsic vulnerability, and several current and potential threats to populations. All three caves occur on protected lands: Bobcat Cave on Redstone Arsenal, Rockhouse Cave on Wheeler National Wildlife Refuge, and Muddy Cave is owned by the Land Trust of North Alabama. Populations face several existing and potential threats. Pollution from surface runoff associated with continued urbanization in the Huntsville metropolitan area and emerging missions and infrastructure projects on Redstone Arsenal threaten cave life, including Spinanycta alabamensis, at all three cave systems (
In many species of the subfamily Cubacubaninae, the area between the 3rd legs and the base of the abdomen has very distinct sexual secondary characters. In Speleonycta ozarkensis, the tibia of third leg has a large bulge with three distinctly long, sclerotized, and curved macrochaetae (
It appears that during reproduction, males in this group may use this part of the body. Evolution has developed a plethora of variable structures. All these structures include some type of chaeta. Sensory input during their interaction with females during courtship may be involved. Unfortunately, their reproductive behavior has yet to be described. Future research may resolve what is the function of all these intriguing structures.
Before the description of S. alabamensis, 9 troglobiotic nicoletiids have been described from caves of Chihuahua and Coahuila in northern Mexico and the United States, including the states of Arkansas, Arizona, Oklahoma, and Texas. At least two undescribed species are known from caves of California. With the discovery of S. alabamensis in Alabama, the distribution of troglobiotic nicoletiids is extended into the Interior Low Plateau karst region in the southeastern United States. Additional diversity may be discovered in the future.
We thank Eric Cline, Brendan Cramphorn, Katie Dooley, Jared Higgs, Joseph Lamb, Eric Maxwell, K. Denise Kendall Niemiller, and Brian Stoltz for assistance with field collection. We thank Christine Easterwood (Redstone Arsenal), William Gates (U.S. Fish & Wildlife Service), Ricky Ingram (U.S. Fish & Wildlife Service), Andy Prewett (Land Trust of North Alabama), Tom Richardson (Redstone Arsenal), Julie Schenck-Brown (Land Trust of North Alabama), Nick Sharp (Land Trust of North Alabama), and Nick Wirwa (U.S. Fish & Wildlife Service) for assistance with collection permits and cave access. Specimens were collected under Alabama Department of Conservation and Natural Resources scientific collection permit nos. 2019060224868680, 2020083527668680, 2021091324068680, 2022096307868680, and 2023109374868680. Sequencing was performed with the help of students of the Fall 2021 BIOL320 Genetics course at Marist College. This project was supported by the Alabama Department of Conservation and Natural Resources (to MLN), U.S. Geological Survey Southeast Climate Adaptation Science Center (grant no. G22AC00270 to MLN), and the National Science Foundation (award no. 2047939 to MLN). Partial support for the project was also granted by the School of Science at Marist College. Jordi Espinasa reviewed an earlier draft of this manuscript. The project described in this publication was supported by Grant No. G22AC00270 from the United States Geological Survey. Its contents are solely the responsibility of the authors and do not necessarily represent the views of the Southeast Climate Adaptation Science Center or the USGS. This manuscript is submitted for publication with the understanding that the United States Government is authorized to reproduce and distribute reprints for Governmental purposes.