Subterranean Biology 13: 1–16, doi: 10.3897/subtbiol.13.6460
Traversing worlds - Dispersal potential and ecological classification of Speolepta leptogaster (Winnertz, 1863) (Diptera, Mycetophilidae)
Dorian D. Dörge 1, Stefan Zaenker 2, Annette Klussmann-Kolb 1, Alexander M. Weigand 1
1 Institute for Ecology, Evolution and Diversity, Goethe-University, Max-von-Laue Str. 13, 60438 Frankfurt am Main, Germany
2 Hesse Federation for Cave and Karst Research, Königswarter Str. 2a, 36039 Fulda, Germany

Corresponding author: Dorian D. Dörge (ggad@hotmail.com)

Academic editor: O. Moldovan

received 18 October 2013 | accepted 13 January 2014 | Published 25 February 2014
(C) 2014 Dorian D. Dörge. 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.
For reference, use of the paginated PDF or printed version of this article is recommended.

Citation: Dörge DD, Zaenker S, Klussmann-Kolb A, Weigand AM (2014) Traversing worlds - Dispersal potential and ecological classification of Speolepta leptogaster (Winnertz, 1863) (Diptera, Mycetophilidae). Subterranean Biology 13: 1–16. doi: 10.3897/subtbiol.13.6460

Abstract

Speolepta leptogaster (Winnertz, 1863) is frequently occurring in European subterranean environments. As for most cave animals, studies addressing non-anatomical aspects are sparse. Here we present the first molecular study on S. leptogaster. We investigated the demographic structure (i.e. COI locus) of 69 specimens from 36 underground populations in Hesse (Central German Uplands) to get first insights into the species’ dispersal ability.

In total, 14 haplotypes were revealed. Haplotype diversity was relatively high, whereas nucleotide diversity was low. Furthermore, a significant but low pattern of isolation-by-distance and (a) past population expansion event(s) were detected.

Our genetic results suggest a (good) active dispersal ability for Speolepta leptogaster. The occurrence of several surface records of adult specimens corroborates this hypothesis. We discuss the developmental stages of S. leptogaster in the context of the ecological classification system and regard the species as a eutroglophile. Evidence has been found to distinguish two larval types. A reconstructed life-cycle of the species is provided.

Keywords

Cave animal, ecotone, phylogeography, mobility, ecological versatility

Introduction

Century and a half have passed since the mycetophilid Speolepta leptogaster (Winnertz, 1863) (Diptera, Mycetophilidae) has been described. The species is widely distributed throughout Europe and can complete its entire life-cycle in subterranean environments such as caves, mines or related underground habitats. Originally placed into the genus Polylepta, Edwards (1925) established the monotypic genus Speolepta in reference to its subterranean ecology and morphology. Due to its enigmatic ecology, obligate subterranean larvae spinning silk-nets and the short adult life spans, Speolepta leptogaster received popular attention amongst entomologists (Schmitz 1912, Lengersdorf and Mannheims 1951, Matile 1962, Plachter 1981). As a tribute, the species was chosen as the Cave Animal of the Year 2013 in Germany. Despite all the scientific attention, research primarily focused on morphological investigations of the different developmental stages (egg, larval stages, pupa and imago) (Schmitz 1912, Lengersdorf and Mannheims 1951, Matile 1962, Plachter 1981), rather than on biological or ecological characteristics. As recently as 2012, two other Speolepta species have been described, thus increasing the number of known species in this genus up to three (Sevcik et al. 2012). In their taxonomic revision, Sevcik et al. (2012) pointed to neglected investigations concerning the species’ dispersal ability. They suggested that “[a]lthough the European Speolepta leptogaster normally breeds and completes its life-cycle entirely underground (Matile 1962), adults of both sexes are frequently found far away from caves. […] This suggests good dispersal abilities where some gene flow may be retained between otherwise very isolated cave populations”.

Here, we investigate the dispersal ability of Speolepta leptogaster by integrating population genetic data of specimens collected from underground sites in the Central German Uplands (Hesse). The study region was chosen since it was covered by permafrost during the Last Glacial Maximum (18, 000 – 24, 500 ybp) (Clark et al. 2009). A postglacial (re-)colonization of this area (inferring a certain level of mobility) rather than the survival in a central German glacial refugium is likely.

Methods
Material and morphological analyses

In total, 69 specimens of Speolepta leptogaster from 37 different caves, bunkers, wells, tunnels and cellars in Hesse (maximum of three per site) and one from a bunker in Poland were analyzed. The samples (Table 1) were collected and identified by members of the Hesse Federation for Cave and Karst Research (Germany) (Reiss et al. 2009) and stored in ethanol. In order to ensure good DNA preservation, all molecularly-processed samples were dated no later than six years old. Prior to DNA isolation, images of all specimens were taken with the camera “Moticam Model Moticam 5“. Specimens were measured using the measuring function of the image-capturing program “Motic Images Plus 2.0”. The bodies of the specimens were examined to determine potential differences in phenotype, which could correspond to different haplotypes.

Table 1.

Dataset of analyzed specimens of Speolepta leptogaster and locality information. LS: life stage (L: larva, P: pupa, I: imago); H: haplotype. The geographic coordinates are in Degrees (°), Minutes (‘) and Decimal seconds (“). The locality numbers resemble the numbers given to each natural region by the German Bundesamt für Naturschutz.

# LS Coordinates Biotope Locality numbers H NCBI
1a L 50°10'13.80"N, 9°24'11.92"E natural cave 141 Sandsteinspessart 9 KF624625
1b L 50°10'13.80"N, 9°24'11.92"E natural cave 141 Sandsteinspessart 1 KF624626
1c L 50°10'13.80"N, 9°24'11.92"E natural cave 141 Sandsteinspessart 4 KF624627
2a L 50°15'49.43"N, 9°31'39.86"E natural cave 141 Sandsteinspessart 1 KF624628
2b L 50°15'49.43"N, 9°31'39.86"E natural cave 141 Sandsteinspessart 1 KF624629
3a I 50°4'55.99"N, 7°48'56.02"E mine shaft 304 Westlicher Hintertaunus 1 KF624630
3b I 50°4'55.99"N, 7°48'56.02"E mine shaft 304 Westlicher Hintertaunus 1 KF624631
4a P 50°5'34.37"N, 7°51'6.16"E mine shaft 304 Westlicher Hintertaunus 8 KF624632
4b L 50°5'34.37"N, 7°51'6.16"E mine shaft 304 Westlicher Hintertaunus 8 KF624633
5a L 50°6'36.32"N, 7°56'49.81"E mine shaft 304 Westlicher Hintertaunus 2 KF624634
5b L 50°6'36.32"N, 7°56'49.81"E mine shaft 304 Westlicher Hintertaunus 2 KF624635
5c L 50°6'36.32"N, 7°56'49.81"E mine shaft 304 Westlicher Hintertaunus 2 KF624636
6 L 50°9'19.87"N, 8°4'53.98"E mine shaft 304 Westlicher Hintertaunus 1 KF624637
7a L 50°52'40.73"N, 8°28'11.28"E mine shaft 320 Gladenbacher Bergland 7 KF624638
7b L 50°52'40.73"N, 8°28'11.28"E mine shaft 320 Gladenbacher Bergland 7 KF624639
8 L 50°53'21.05"N, 8°25'39.54"E mine shaft 320 Gladenbacher Bergland 11 KF624640
9 L 50°52'23.23"N, 8°28'37.34"E rock cellar 320 Gladenbacher Bergland 3 KF624641
10a L 51°0'4.61"N, 8°35'41.53"E mine shaft 332 Ostsauerländer Gebirgsrand 2 KF624642
10b L 51°0'4.61"N, 8°35'41.53"E mine shaft 332 Ostsauerländer Gebirgsrand 2 KF624643
10c L 51°0'4.61"N, 8°35'41.53"E mine shaft 332 Ostsauerländer Gebirgsrand 2 KF624644
11a L 51°23'34.73"N, 8°41'28.79"E mine shaft 332 Ostsauerländer Gebirgsrand 1 KF624645
11b L 51°23'34.73"N, 8°41'28.79"E mine shaft 332 Ostsauerländer Gebirgsrand 14 KF624646
11c L 51°23'34.73"N, 8°41'28.79"E mine shaft 332 Ostsauerländer Gebirgsrand 1 KF624647
12a L 51°13'56.89"N, 8°54'4.32"E natural cave 340 Waldecker Tafelland 2 KF624648
12b L 51°13'56.89"N, 8°54'4.32"E natural cave 340 Waldecker Tafelland 2 KF624649
13a L 51°14'25.08"N, 8°54'9.40"E mine shaft 340 Waldecker Tafelland 1 KF624650
13b L 51°14'25.08"N, 8°54'9.40"E mine shaft 340 Waldecker Tafelland 1 KF624651
14 L 51°18'55.58"N, 9°24'26.86"E undercroft 342 Habichtswälder Bergland 1 KF624652
15a L 51°7'41.70"N, 8°59'0.17"E spring 344 Kellerwald 1 KF624653
15b L 51°7'41.70"N, 8°59'0.17"E spring 344 Kellerwald 1 KF624654
16 L 51°7'32.66"N, 8°59'33.47"E spring 344 Kellerwald 1 KF624655
17 L 50°30'3.56"N, 9°7'25.43"E rock cellar 350 Unterer Vogelsberg 1 KF624656
18a L 50°31'0.59"N, 9°32'3.73"E mine shaft 350 Unterer Vogelsberg 1 KF624657
18b L 50°31'0.59"N, 9°32'3.73"E mine shaft 350 Unterer Vogelsberg 1 KF624658
19 I 50°27'0.29"N, 9°49'15.92"E rock cellar 353 Vorder- und Kuppenrhön 2 KF624659
20 L 50°34'21.18"N, 9°57'38.63"E rock cellar 353 Vorder- und Kuppenrhön 12 KF624660
21 L 50°35'23.96"N, 9°59'54.13"E rock cellar 353 Vorder- und Kuppenrhön 1 KF624661
22a P 50°35'57.73"N, 9°59'59.60"E culvert 353 Vorder- und Kuppenrhön 1 KF624662
22b P 50°35'57.73"N, 9°59'59.60"E culvert 353 Vorder- und Kuppenrhön 1 KF624663
23a L 50°30'30.64"N, 9°55'48.65"E mine shaft 354 Hohe Rhön 1 KF624664
23b L 50°30'30.64"N, 9°55'48.65"E mine shaft 354 Hohe Rhön 6 KF624665
23c L 50°30'30.64"N, 9°55'48.65"E mine shaft 354 Hohe Rhön 6 KF624666
24a L 50°28'7.25"N, 9°57'45.40"E spring 354 Hohe Rhön 1 KF624667
24b L 50°28'7.25"N, 9°57'45.40"E spring 354 Hohe Rhön 1 KF624668
25a L 50°52'35.18"N, 9°42'27.40"E brick-built cellar 355 Fulda-Haune-Tafelland 1 KF624669
25b L 50°52'35.18"N, 9°42'27.40"E brick-built cellar 355 Fulda-Haune-Tafelland 1 KF624670
26a L 50°53'4.56"N, 9°43'25.10"E rock cellar 355 Fulda-Haune-Tafelland 1 KF624671
26b L 50°53'4.56"N, 9°43'25.10"E rock cellar 355 Fulda-Haune-Tafelland 1 KF624672
27a L 50°51'35.21"N, 9°45'19.94"E mine shaft 355 Fulda-Haune-Tafelland 1 KF624673
27b L 50°51'35.21"N, 9°45'19.94"E mine shaft 355 Fulda-Haune-Tafelland 13 KF624674
27c L 50°51'35.21"N, 9°45'19.94"E mine shaft 355 Fulda-Haune-Tafelland 1 KF624675
28a L 51°7'34.36"N, 9°47'35.70"E brick-built tunnel 357 Fulda-Werra-Bergland 1 KF624676
28b L 51°7'34.36"N, 9°47'35.70"E brick-built tunnel 357 Fulda-Werra-Bergland 10 KF624677
29 L 51°12'26.24"N, 9°52'16.82"E mine shaft 357 Fulda-Werra-Bergland 1 KF624678
30 L 51°0'43.13"N, 9°55'45.73"E mine shaft 357 Fulda-Werra-Bergland 1 KF624679
31a L 51°0'24.88"N, 9°57'44.68"E mine shaft 357 Fulda-Werra-Bergland 5 KF624680
31b L 51°0'24.88"N, 9°57'44.68"E mine shaft 357 Fulda-Werra-Bergland 5 KF624681
31c L 51°0'24.88"N, 9°57'44.68"E mine shaft 357 Fulda-Werra-Bergland 5 KF624682
32a L 51°13'29.10"N, 9°57'8.68"E mine shaft 358 Unteres Werratal 1 KF624683
32b L 51°13'29.10"N, 9°57'8.68"E mine shaft 358 Unteres Werratal 1 KF624684
33a L 51°13'27.05"N, 9°57'11.74"E touristic mine 358 Unteres Werratal 2 KF624685
33b L 51°13'27.05"N, 9°57'11.74"E touristic mine 358 Unteres Werratal 2 KF624686
34a L 51°10'45.44"N, 10°4'15.28"E mine shaft 358 Unteres Werratal 1 KF624687
34b L 51°10'45.44"N, 10°4'15.28"E mine shaft 358 Unteres Werratal 1 KF624688
35 L 51°31'8.11"N, 9°22'39.43"E bunker complex 361 Oberwälder Land 1 KF624689
36a L 51°31'8.11"N, 9°22'39.43"E bunker complex 361 Oberwälder Land 1 KF624690
36b L 51°31'8.11"N, 9°22'39.43"E bunker complex 361 Oberwälder Land 1 KF624691
36c L 51°31'8.11"N, 9°22'39.43"E bunker complex 361 Oberwälder Land 1 KF624692
37 I 52°24'0"N, 15°31'59.99"E bunker complex Nietoperek (Poland) 8 KF624693
Σ 69
Molecular analyses

A small piece of the posterior end of the body (approx. one sixth of the total animal) was used for larval samples. In the case of pupae and imagines, a larger portion of the abdomen (approx. ¼) was macerated. DNA isolation was performed according to the instructions of the DNEasy Blood & Tissue Kit (Qiagen Sample and Assay Technologies, Hilden, Deutschland) for the column purification of animal tissue.

A 662 bp fragment of the Cytochrome C Oxidase subunit 1 (COI) gene was amplified using the primers C1-J-2195 5’-TTGATTTTTTGGTCACCCTGAAGT-3’ and TL2-N-3014 5’-TCCAATGCACTAATCTGCCATATTA-3’ established by Simon et al. (1994). The PCR reactions were executed in a Peqlab Primus Advanced 96 thermo cycler. Each PCR-mix (25 µL) contained 2.5 µL PCR-buffer (10×, without MgCl2), 2.0 µL MgCl2 (100 mM), 0.3 µL dNTPs (20 mM), 1.0 µL of each primer, 0.3 µL Taq-DNA-Polymerase, 1.5 µL BSA (bovine serum albumin, 10 mg/mL), 11.4 µL ddH2O and 5.0 µL template DNA. PCR conditions were as follows: initial denaturation step 1 min 94 °C, 30 cycles of denaturation (30 sec, 94 °C), annealing (30 sec, 43.7 °C) and elongation (30 sec, 72 °C) and a final elongation step with 7 min at 72 °C. PCR products were bi-directionally sequenced using the Sanger chain termination method (Sanger et al. 1977). Sequencing service was provided by the Laboratory Centre of the Biodiversity and Climate Research Centre (Frankfurt am Main, Germany) with their own sequencing protocols. Editing and assembly of the forward and reverse sequences were done using Geneious v5.4.6. The sequences were manually trimmed to a length of 659 bp to fit the shortest sequence retained. Sequence alignment was performed using the MAFFT v6.814b plug-in for Geneious under default settings and the automatic algorithm option.

Population genetic analyses

The software DnaSP v5 (Librado and Rozas 2009) was used to calculate the number of haplotypes, the total haplotype and nucleotide diversity and to perform neutrality tests. Haplotype diversity (Hd) can result in values between 0 and 1. A value of Hd = 1 implies that two randomly picked samples will always demonstrate two different haplotypes (= 100% diversity). The nucleotide diversity (π) illustrates the average genetic distance between two sequences estimated as an average for all sequences. The value can range from 0 (no changes in all sequences) to a theoretical 1 (every base is replaced). The calculation for Fu’s Fs (Fu 1997) and Tajima’s D (Tajima 1989) tests can be positive, negative or have a zero value. A significant positive value for Tajima’s D may point to over dominant selection or a population bottleneck event. Significant negative values point to a population expansion event or purifying selection. A value of zero or non-significant values cannot reject the neutral model of molecular evolution. Fu’s Fs shares the same characteristics but adds the support for genetic hitchhiking with a negative value. Standard settings were used and the sequences were trimmed to the same length. The program TCS 1.21 (Clement et al. 2000) was used to reconstruct a haplotype network by Statistical Parsimony (Templeton et al. 1992). Networks were created by a 95% connection probability.

A Mantel-test (Mantel 1967) was used to test for correlation between geographic distance vs. genetic distance. The geographic distance matrix was calculated with the Geographic Distance Matrix Generator 1.2.3 (Ersts 2014) using a WGS84 spheroid and geodesic distances in km. Genetic distances were calculated as p-distances using the software MEGA 5.2 (Tamura et al. 2011) and the pairwise deletion option. The Mantel-test was performed in XLSTAT 2013 (Addinsoft) using the linear Pearson product-moment correlation coefficient (r) and 10, 000 permutations. A value of r = 0 implies no linear correlation, whereas a minimal / maximal value of -1 / +1 indicates total negative / positive correlation.

Results
Demographic structure of Speolepta leptogaster in Hesse

No gaps were present in the COI-alignment. In total, 14 haplotypes (H1-H14) were revealed. Haplotype diversity was high with a value of Hd = 0.7017, whereas nucleotide diversity was low with π = 0.00165 (Table 2). The haplotype network (Figure 1) indicated a highly frequent haplotype, H1, which consisted of 39 samples (57%) and a second relatively frequent haplotype, H2, which comprised 11 samples (16%). Eight haplotypes were singletons (H3, H4, H9-H14), two consisted of two (H6 and H7) and two of three samples (H5 and H8). There were only four haplotypes (H4, H8, H9 and H11) which were not directly connected to the most frequent haplotype H1.

Figure 1.

CO1 haplotype network for Speolepta leptogaster. Haplotypes are numbered in sequence with their volume proportional to their frequency in the total dataset. Lines interconnecting the haplotypes illustrate the mutational course and the number of mutational steps between them. Numbers with letters within or alongside circles refer to Table 1.

Table 2.

Overview of statistical values. Estimates are given for neutrality tests (Fu’s Fs, Tajima’s D), haplotype (Hd), nucletide diversity (π) and Pearson’s r in a Mantel-test (geographic distance vs. genetic distance).

estimates value p-value
Fu’s Fs -10.28 p < 0.001
Tajima’s D -1.89 p = 0.004
Hd 0.7017
π 0.00165
r 0.17 p < 0.0001

When the different haplotypes are placed in a geographical context (Figure 2), H1 can be revealed throughout the study region of Hesse. Haplotype 2 demonstrates a similar distribution except in the central underground sites and the most northern parts of Hesse. Haplotype 8 occurs once in southern Hesse and in the sampling site in Poland. All other haplotypes have been found within only a single locality. At a few localities several haplotypes co-occurred: In north-western Hesse H14+H1 and H2+H1; in north-eastern Hesse H9+H1, H2+H1 and H13+H1 and in south-eastern Hesse, H10+H6+H1.

Figure 2.

Spatial pattern of haplotypes of Speolepta leptogaster in Hesse. The haplotype (H) distribution of Speolepta leptogaster within Hesse (A) with a comparison group in Poland (B) is depicted as a circle for every underground locality with colored sections for the different haplotypes. To be depicted in a reasonable manner, multiple localities were reduced to one circle if they were situated nearby (up to 4 km) and had the same color.

The results of both neutrality tests were significantly negative (p < 0.01) and point to (a) past population expansion event(s) (Table 2). In our dataset, 28.5% of all mutations (4/14) were non-synonymous leading to a change of the respective amino acid.

The Mantel-test (r = 0.17, p < 0.0001) reveals a significant positive low correlation between genetic distance and geographic distance (Table 2).

Discussion
Dispersal ability

The region of the Central German Uplands (including our target area of Hesse) was covered with permafrost during the Last Glacial Maximum (18, 000 – 24, 500 years ago) (Clark et al. 2009). It is widely accepted, that ecologically diverse species were able to (re-)colonize this area when the climatic conditions became more suitable after the ice shields had retracted northward again (Taberlet et al. 1998, Hewitt 1999, Petit et al. 2002). Our genetic analyses are in agreement with a similar postglacial scenario for Speolepta leptogaster. The recent demographic structure of this species in Hesse is best explained by (a) past population expansion event(s). Most probably and after population bottlenecks, the low-frequency and most often cave endemic haplotypes have evolved from the high-frequency central haplotypes already present in the ancestral gene pool of the species (i.e. the founder effect). The significant but weak pattern of isolation-by-distance can be interpreted in terms of a certain level of connectivity between populations, which may be explained by dispersal of adult specimens. An interesting finding is the identity of haplotypes found in Poland and southern Hesse. Yet, a pan-European sampling is needed to address any further hypotheses (e.g. passive anthropogenic transportation vs. active surface-dispersal).

Box 1.

Original description of Speolepta leptogaster (Winnertz, 1863). Translated from German. Originally this species has been described under the name of Polylepta leptogaster.

The habitus is very similar to the Bolitophila. Body color brown. Mouth-rim slightly pulled forward and garlanded with hairs. The filamentous antennae are about 1.33 times as long as head and thorax together. The flagellum links are 3 to 4 times as long as broad. The haltere is whitish with a black-brown tip. The abdomen is very slim and cylinder-shaped, about 5 to 6 times as long as the very short thorax and constricted at the base. The coxa and femur yellow, tibia more brownish, tarsus light brown. The feet of the front legs are 2.33 times as long as the tibia, the tibia slightly shorter than the metatarsus (9 : 9 ¾) with lanceolate basis. Wings slightly greyish nearly colorless; the subcosta proceeding over the cubitus up to the tip of the wing, the supporting vein broken off in front of the lateral vein, the marginal lateral vein pulled far back, the discal cell trapezoid-shaped, 1.5–2 times as long as broad, the style of the upper fork about half the length of the upper prong, the basis of the rear cell under the middle of the wing on the far side of the discal cell, the axilla vein not sturdy, broken off on the opposite side of the rear cell. I only captured a female of this very rare species once in august in a swampy, forested area. A second female is located at the Royal Museum in Leyden, which differs from mine in the way that the discal cell, which is 1.5 times as long as broad in my specimen, is 2 times as long as broad. Apart from that, they completely matched.

In general, our results imply good dispersal ability for Speolepta leptogaster. This is further supported by surface records of adult specimens compiled from the literature (Table 3). Although all developmental stages can be found in caves throughout the year, there are more findings of surface imagines in summer than in winter. Whether this is due to the biology of Speolepta leptogaster or to the smaller number of traps being laid out in winter cannot be determined.

Table 3.

Surface records of Speolepta leptogaster. N: number of specimens found, f: female, m: male.

Region Date of collection Habitat/collection N Reference
swampy forest area 1 f Winnertz (1863)
Germany, Birgsau, südlich von Oberstdorf, im Stillachtal 18–27 Sept. 1975 light trap 1 m Plassmann (1977), first description Speolepta dissona
Germany, Saxon Switzerland 1.5 km SE of Obervogelgesang 10–21 May 1997 deciduous forest, Malaise trap 1 f, 1 m U. Kallweit (unpublished)
S-Germany, Grenzach 11 May 2008 1 f B. Rulik (unpublished)
Germany, Harz mountains 26 Oct. 2004 natural mature spruce forest, yellow pan trap 2 m U. Kallweit (unpublished)
Germany, Harz mountains 25 June 2004 natural mature spruce forest, Malaise trap 1 m U. Kallweit (unpublished)
Germany, Hesse, Fulda, Mittelbergquelle 10 Oct. 2004 hand collection 1 f Zaenker (2008)
Germany, Hesse, Auersbergquelle 21 18 Sept. 2009 sweep net 1 f Zaenker unpublished
Germany, Hesse, Lützeler Sang-Quelle 2 25 Oct. 2007 sweep net 1 m Zaenker (2008)
Norway, Kvinnherad, Rosendal, riverside at Avlsgården, Baroniet 11–15 May 1990 Malaise trap 1 f, 2 m Ševčík et al. (2012)
Norway, Bergen, 9 May–28 June 1991 Malaise trap 3 m Ševčík et al. (2012)
Haukeland
Norway, Bømlo, Vorland, Langevåg 11 Feb 2002–12 Feb 2003 Malaise trap 7 f, 5 m Ševčík et al. (2012)
Norway, Etne, Skånevik skyttarbane 3 Sept. 2009 sweep net 1 f, 1 m Ševčík et al. (2012)
Norway, Fjell, Vindenes 5 Sept. 1978 light trap 1 f Ševčík et al. (2012)
Norway, Os, Raudli 23–30 May 1991 1 f, 1 m Ševčík et al. (2012)
Norway June–Sept. 1991 Malaise trap 17 f, 11 m Ševčík et al. (2012)
Norway, Os, Sæleli 20–27 June 1991 Malaise trap 1 m Ševčík et al. (2012)
Norway, Øygarden, Dalsvann, Alvøy 5 June 1987 light trap 1 f Ševčík et al. (2012)
Norway, Sveio, Førde, Solheimshaugen 3–10 June 1991 Malaise trap 2 f Ševčík et al. (2012)
Norway, Sveio, Førde, Solheimshaugen 15 June 1991 sweep net 1 f, 1 m Ševčík et al. 2012
Norway, Sunndal, 31 Mai–13 Jul. & 26 Aug.–6 Sept. 2004 Malaise trap 9 f, 14 m Ševčík et al. (2012)
Jordalsgrenda, Jordalsøra, Hamrene
Norway, Sunndal, 14 June–3 Jul. & 12–25 Aug. 2005 window trap 1 f, 1 m Ševčík et al. (2012)
Jordalsgrenda, Jordalsøra, Hamrene
Norway, Aurland, Vassbygdvatnet 4 Aug. 1969 sweep net 1 f Ševčík et al. (2012)
(lower end of lake)
Norway, Porsgrunn, Hitterødbekken 13 June–11 Jul. 1988 Malaise trap 3 f Ševčík et al. (2012)
Sweden, Jokkmokk, 19–30 June 1968 air suction trap 1 f, 3 m Ševčík et al. (2012)
Kaltisbäcken 1 km NNE Messaure
Sweden, Lund, Høje Å (stream) at Värpinge 23–28 May 2004 yellow pan trap 1 m Ševčík et al. (2012)
Sweden, Klippan, 26 Sept. 1983 sweep net 1 m Ševčík et al. (2012)
Skäralid NR (ravine with stream)
Sweden, Högsby kommun, 29 Jul–31 Aug. 2004 Malaise trap 1 f Ševčík et al. (2012)
Getebro
Faroe Islands, Streymoy, 13–17 Jul. 1990 Malaise trap 2 m Ševčík et al. (2012)
Kvivik
Czech Republic, Bohemia, Jizerské Hory Mts, Jedlový důl 6–28 Jul. & 1–22 Sept. 2005 Malaise trap 3 m Ševčík et al. (2012)
Czech Republic, Bohemia, Mt. Poledník 29 Aug. - 5 Okt. 2004 Malaise trap 1 m Ševčík et al. (2012)
Czech Republic, Bohemia, Krkonoše Mts., Bílé Labe 16–30 Aug. 2007 Malaise trap 1 m Ševčík et al. (2012)
Czech Republic, Bohemia, Labský důl 24–27 Jul. 2006 Malaise trap 1 m Ševčík et al. (2012)
Czech Republic, Moravia & Silesia, Hrubý Jeseník Mts, Velká kotlina 9–26 June 2006 Malaise trap 1 m Ševčík et al. (2012)
Czech Republic, Moravia & Silesia, Rejvíz 20 May–1 Jul. 2005 peat-bog, Malaise trap 1 f Ševčík et al. (2012)
Slovakia, Pol’ana Mts., Hrončecký grún 7 May–4 Jul. 2006 yellow pan trap 1 m Ševčík et al. (2012)
Slovakia, Kyslinky–Pod Dudášom 15 June 2009 1 m Ševčík et al. (2012)
Slovakia, Predná Pol’ana Mt.–Bystré waterfall 17 June 2009 1 m Ševčík et al. (2012)
Slovakia, Spády waterfall 18 June & 4 Jul. 2009 2 m Ševčík et al. (2012)
[52 f, 64 m]
Ecological classification

Animals associated with underground habitats can be classified into different categories. Those classifications (i.e. ecological, behavioral, morphological) have been under constant change and revision. Multiple authors created new categories as well as split up old ones (Shiner 1854, Racovitza 1907, Vandel 1965, Hamilton-Smith 1971, Sket 2008). However, the main ecological categories to which we refer here have remained more or less unchanged: eutrogloxenes (normally not living in caves), subtroglophiles (partially living in caves, but without permanent populations), eutroglophiles (able to complete several underground generations) and eutroglobionts (solely living in caves). As a result of this ecological continuum of cave-association, i.e. from “only found by chance” to “being obligate subterranean”, probable cave-associated (e.g. morphological and behavioral) adaptations are multifarious.

Since the biological diversity of subterranean species and ecology of subterranean habitats is high (Moseley 2008), every categorical and thus limited ecological classification system will elicit problems in classifying all cave organisms. This is particularly challenged by a “species from both worlds” living in a transitional environment or ecotone, as which caves must be considered (Moseley 2008). The situation is even more complicated by the fact that Speolepta leptogaster belongs to the holometabolic insects with different developmental stages demonstrating different ecological requirements. This species is thus a prime example that an ecological classification system for cave-dwelling species, based on four categories may be too ambiguous particularly in cases where different life stages may behave ecologically distinct. Here we discuss the species three effective life stages, including the larva, pupa and imago in respect to the ecological classification system. We characterize the single developmental stages and potentially the whole species.

The larvae hatch and live solely within subterranean habitats reaching from microcavities to macrocaverns (or caves). They are incapable of surviving on the surface, which is related to their preference for a highly water-saturated atmosphere and adaptation to oxygen respiration. They lack a trachea system but are able to respire oxygen through a very thin cuticula spanning the entire body surface (Schmitz 1912). Author’s observations (SZ and AW) point to a behavior of avoiding strong air currents. Since the pupal stage is immobile and directly succeeds the larval developmental stage, it can only occur in the same habitat. The imago however, possesses elongated legs (sometimes regarded as a troglomorphy) (Schönborn 2003) and demonstrates a sluggish flight. At the same time, imagines do not feed and probably only survive a few days to weeks, thus complicating the inference of their ability to survive outside the subterranean habitat. However, several surface records of imagines (Table 3) and sightings of larvae in the transition and entrance zones of underground sites (Zaenker 2008, Weber 2012) are known. Furthermore, it seems that adult specimens travel between caves during the night.

Conclusively, not all developmental stages are capable of surviving outside the subterranean zone. Thus, the completion of a life-cycle aboveground will be incomplete – eliminating the eutrogloxenes as a potential ecological category for Speolepta leptogaster. Due to the short life-span of adults rarely leaving the subterranean zone, the complete life-cycle (or a very large proportion) is within the subterranean environment – leaving the eutroglophiles and eutroglobionts. From an evolutionary point of view and for long-term survival, Speolepta leptogaster should be classified as a eutroglophile, i.e. being able to complete several underground generations but having the ability of surface dispersal. But pinpointing Speolepta leptogaster to a single ecological category clearly underestimates the ecological versatility of the species.

Potential life-cycle

Even after 150 years, some facts about the biology of Speolepta leptogaster are still unknown. Specifically, these include the number of larval stages and the durations of the different life stages. Although Schmitz (1912) claimed that he had successfully bred Speolepta leptogaster in captivity, he provided no information about the duration of any of the life stages. Still, a comparison with related Mycetophilidae (including the ecologically-similar keroplatid Arachnocampa luminosa (Skuse, 1890)) (Baker 2010, Li et al. 2011) may enable a vague picture of the potential life-cycle and the life-spans of the different developmental stages: a) egg: approx. 2 weeks; b) larval stages: 6 – 12 months; c) pupa: approx. 2 weeks and d) imago: 4 – 20 days (Figure 3).

Figure 3.

Potential life-cycle of Speolepta leptogaster; egg-drawing modified after the descriptions of Plachter (1981).

Two types of larvae were present in our material. They can be distinguished by a small deviance of the ocelli position and by body measurements (Figure 4). In type A, the ocellus is situated adjacent to the antenna whereas in type B, the ocellus is approximately 15 to 20 µm behind the antenna. The head capsule of larvae type B was thinner (A: about 210 µm, B: about 190 µm), slightly shorter (A: about 300 µm, B: about 280 µm) and generally more pointed than in type A. The labrum of larvae type B displays a deeper indentation in the middle of the frontal end. At the proximal end of the head area where the vermiform body begins, the larvae type A displays an edged transition, whereas with larvae type B, it is more semicircular. In the sample set, three larvae were found that appeared as depicted in type B. Two of which had only half the total length of the average length of a normal larva (4.7 mm and 5.0 mm compared to 10 mm). A third specimen was of normal size. Since different larval stages between hatching and pupating are reported in other Mycetophilidae (Madwar 1937), this might explain the morphological discrepancy of larval type A and B in Speolepta leptogaster.

Figure 4.

Comparison between two larval stages of Speolepta leptogaster. A depicts the larger and probably older larva type A which on average is 10 mm long B depicts the smaller larva B type which is 5–10 mm long. Dotted regions depict areas of increased pigmentation, black regions illustrate maximum pigmentation.

Conclusions

Since this work presents the first step towards understanding the dispersal potential of the ecologically versatile species Speolepta leptogaster within a small area, subsequent studies should incorporate a larger, pan-European sampling to address diversification patterns for this abundant cave species. Its ecological diversity in congruence with frequent subterranean and sporadic surface animals further challenges the eco-categorical classification system applied for subterranean species.

Acknowledgements

Images of pupa and the male imago were taken by Klaus Bogon. We thank all members of the Hesse Federation for Cave and Karst Research for sample collection, Adrienne Jochum for proofreading the manuscript and two anonymous reviewers for their constructive comments.

References
Baker CH (2010) A new subgenus and five new species of Australian glow-worms (Diptera: Keroplatidae: Arachnocampa). Memoirs of the Queensland Museum 55(1): 11-41.
Clark PU, Dyke AS, Shakun JD, Carlson AE, Clark J, Wohlfahrth B, Mitrovica JX, Hostetler SW, McCabe AM (2009) The Last Glacial Maximum. Science 325(5941): 710-714. doi: 10.1126/science.1172873
Clement M, Posada D, Crandall K (2000) TCS: a computer program to estimate gene genealogies. Molecular Ecology 9(10): 1657-1660. doi: 10.1046/j.1365-294x.2000.01020.x
Edwards FW (1925) British fungus-gnats (Diptera, Mycetophilidae). With a revised generic classification of the family. Transactions of the Royal Entomological Society of London 1925: 505-670.
Ersts PJ (2014) Geographic Distance Matrix Generator (version 1.2.3). American Museum of Natural History, Center for Biodiversity and Conservation. http://biodiversityinformatics.amnh.org/open_source/gdmg [accessed on 2014-1-5]
Fu YX (1997) Statistical tests of neutrality of mutations against population growth, hitch-hiking, and background selection. Genetics 147(2): 915-925.
Hamilton-Smith E (1971) The classification of Cavernicoles. National Speleological Society Bulletin 33: 63-66.
Hessisches Landesamt für Umwelt und Geologie: Umweltatlas Hessen - Die Naturräume Hessens und ihre Haupteinheiten http://atlas.umwelt.hessen.de
Hewitt GM (1999) Post-glacial re-colonization of European biota. Biological Journal of the Linnean Society 68: 87-112. doi: 10.1111/j.1095-8312.1999.tb01160.x
Lengersdorf F, Mannheims BB (1951) Das kleine Fliegenbuch: von heimischen Fliegen und Mücken. Reitter 30–33.
Librado P, Rozas J (2009) DNASP v5: A software for comprehensive analysis of DNA polymorphism data. Bioinformatics 25: 1451-1452. doi: 10.1093/bioinformatics/btp187
Li X-Z, Niu C-Y, Huang Q-Y, Lei C-L, Stanley DW (2011) Life cycle of Chetoneura shennonggongensis (Diptera: Keroplatidae: Keroplatinae) from Jiangxi Province, China. Insect Science 16: 351-359.
Madwar S (1937) Biology and Morphology of the immature stages of Mycetophilidae (Diptera: Nematocera). Philosophical Transactions of the Royal Society of London Series B, Biological Sciences 227: 1-110. doi: 10.1098/rstb.1937.0001
Mantel N (1967) The detection of disease clustering and a generalized regression approach. Cancer Research 27(2): 209-220.
Matile L (1962) Morphologie et biologie d’un insecte diptere cavernicole Speolepta leptogaster Winnertz (Mycetophilidae). Mémoires du Museum National d’Histoire Naturelle 20: 219–242.
Moseley M (2008) Size matters: scalar phenomena and a proposal for an ecological definition of ‘cave’. Cave and Karst Science 35(3): 89-94.
Petit RJ, Brewer S, Bordács S, Burg K, Cheddadi R, Coart E, Cottrell J, Csaikl UM, van Dam B, Deans JD, Espinel S, Fineschi S, Finkeldey R, Glaz I, Goicoechea PG, Jensen JS, König AO, Lowe AJ, Madsen SF, Mátyás G, Munro RC, Popescu F, Slade D, Tabbener H, de Vries SGM, Ziegenhagen B, de Beaulieu JL, Kremer A (2002) Identification of refugia and post-glacial colonisation routes of European white oaks based on chloroplast DNA and fossil pollen evidence. Forest Ecology and Management 156(1–3): 49-74. doi: 10.1016/S0378-1127(01)00634-X
Plachter H (1981) Chorionic structures of the eggshells of 15 Fungus- and Root-gnat species (Diptera: Mycetophilidae). International Journal of Insect Morphology and Embryology 10: 43-63. doi: 10.1016/0020-7322(81)90012-X
Racovitza EG (1907) Éssai sur les problèmes biospéologiques (Biospeologica, 1). Archives de Zoologie Experimentale et Génerale, 4e série 6: 371–488.
Reiss M, Steiner H, Zaenker S (2009) The Biospeleological Register of the Hesse Federation for Cave and Karst Research (Germany). Cave and Karst Science 35(1): 25-34.
Sanger F, Nicklen S, Coulson AR (1977) DNA sequencing with chain-terminating inhibitors. Proceedings of the National Academy of Sciences 74(12): 5463-5467. doi: 10.1073/pnas.74.12.5463
Schmitz H (1912) Biologisch-anatomische Untersuchungen an einer höhlenbewohnenden Mycetophilidenlarve, Polylepta leptogaster Winn. Jaarboek van het Natuurhistorisch Genootschap in Limburg 65–96.
Schönborn W (2003) Lehrbuch der Limnologie. Schweizerbartsche Verlagsbuchhandlung.
Ševčík J, Kjærandsen J, Marshall SA (2012) Revision of Speolepta (Diptera: Mycetophilidae), with descriptions of new Nearctic and Oriental species. The Canadian Entomologist 144(1): 93-107. doi: 10.4039/tce.2012.10
Simon C, Frati F, Beckenbach A, Crespi B, Liu H, Flook A (1994) Evolution, weighting, and phylogenetic utility of mitochondrial gene sequence and compilation of conserved polymerase chain reaction primers. Annals of the Entomological Society of America 87: 651-701.
Sket B (2008) Can we agree on an ecological classification of subterranean animals? Journal of Natural History 42(21–22): 1549–1563. doi: 10.1080/00222930801995762
Skuse FAA (1890) Description of a luminous dipterous insect (Fam. Mycetophilidae), from New Zealand. Proceedings of the Linnean Society of New South Wales (second series) 5: 677-679.
Taberlet P, Fumagalli L, Wust-Saucy AG, Cosson JF (1998) Comparative phylogeography and postglacial colonization routes in Europe. Molecular Ecology 7: 453-464. doi: 10.1046/j.1365-294x.1998.00289.x
Tamura K, Peterson D, Peterson N, Stecher G, Nei M, Kumar S (2011) MEGA5: molecular evolutionary genetics analysis using maximum likelihood, evolutionary distance, and maximum parsimony methods. Molecular biology and evolution 28(10): 2731-2739. doi: 10.1093/molbev/msr121
Tajima F (1989) Statistical method for testing the neutral mutation hypothesis by DNA polymorphism. Genetics 123(3): 585-595.
Templeton AR, Crandall KA, Sing CF (1992) A cladistic analysis of phenotypic associations with haplotypes inferred from restriction endonuclease mapping and DNA sequence data. III. Cladogram estimation. Genetics 132(2): 619-633.
Vandel A (1965) Biospeleology, the Biology of cavernicolous animals. Pergamon Press, Oxford, 524 pp.
Weber D, Zaenker S, Plassmann E (2007) Pilzmücken in Höhlen und künstlichen Hohlräumen (Diptera: Sciaroidea: Ditomyiidae, Bolitophilidae, Diadocidiidae, Keroplatidae, Mycetophilidae). Entomofauna 28(11): 125-140.
Weber D (2012) Die Höhlenfauna und -flora des Höhlenkatastergebietes Rheinland-Pfalz/Saarland, 5. Teil. Abhandlungen zur Karst- und Höhlenkunde 36.
Winnertz J (1863) Beitrag zu einer Monografie der Pilzmücken (Mycetophilidae). Verhandlungen der Zoologisch-Botanischen Gesellschaft in Wien 13: 637-964.
Zaenker S (2008) Das Biospeläologische Kataster von Hessen. Abhandlungen zur Karst- und Höhlenkunde 32. [Fortschreibung zum 12.04.2008]