Quasicalathus conservans Schmidt & Will, 2022
publication ID |
https://dx.doi.org/10.3897/dez.69.79931 |
publication LSID |
lsid:zoobank.org:pub:02E8488B-DDA7-464C-ABC2-39424200939E |
persistent identifier |
https://treatment.plazi.org/id/1EAF9667-E896-445B-ADED-0DA2B055DF2B |
taxon LSID |
lsid:zoobank.org:act:1EAF9667-E896-445B-ADED-0DA2B055DF2B |
treatment provided by |
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scientific name |
Quasicalathus conservans Schmidt & Will |
status |
sp. nov. |
Quasicalathus conservans Schmidt & Will sp. nov.
Material studied.
Male in Rovno amber, with specimen label data " SDEI-Amb-002529 ", deposited in the Senckenberg Deutsches Entomologisches Institut, Müncheberg, Germany. Size of the amber piece 20 × 10 × 8.5 mm.
Preservation status: The amber is clear but pervaded by numerous small air bubbles and extensive flowlines attached to the embedded fossil that is therefore only partly visible using light microscopy (Figs 32 View Figures 31–33 , 33 View Figures 31–33 ). The exoskeleton of the fossil, including most parts of the aedeagus, is well preserved and, therefore, important diagnostic characters could be reconstructed using micro-CT (Figs 78 View Figures 78–80 - 89 View Figures 81–89 ).
Syninclusions: One stellate hair, few tiny dust particles.
Description.
Measurements see Table 2 View Table 2 .
Standardized body length: 7.3 mm.
Proportions: A3L/HL = 0.44;
EyL/ HW(-) = 0.72;
PW/HW(+) = 1.40;
PW/PL = 1.27;
PW/PWb = 1.11;
PWb/PWa = 1.46;
EW/PW = 1.64;
EL/EW = 1.51;
EpL/EpW = 1.43;
EL/FL = 2.58;
EL/AedL = 3.64.
Head: As described in Q. elpis .
Prothorax: Pronotal lateral margin moderately narrowed toward base, slightly concave before laterobasal angles, angles slightly obtuse (Fig. 78 View Figures 78–80 ). Prosternal process with traces of a lateral bead (Fig. 85 View Figures 81–89 ). In all other characters as described for the new genus, above.
Pterothorax: Elytra with basal margin markedly concave and humerus markedly protruded anteriorly; basal margin forming a slightly obtuse angle (ca. 115°) with the lateral margin (Fig. 78 View Figures 78–80 ). Elytral striae moderately deeply engraved, intervals moderately convex. In all other characters as described for the new genus, above.
Aedeagus: Length of median lobe about 1.33 mm; median lobe terminal lamella moderately long, almost evenly narrowed from base to apex (Fig. 88 View Figures 81–89 ); terminal lamella almost straight, with tip very slightly bent ventrally (Figs 87 View Figures 81–89 , 89 View Figures 81–89 ). In all other characters as described for the new genus, above.
Differential diagnosis.
In external characters, Q. conservans sp. nov. appears identical to Q. elpis , however, it can be distinguished by the male genitalia. The new species differs by the proportionally larger aedeagus (EL/AedL = 3.64 instead of 4.05 in Q. elpis ) and by the shape of the median lobe terminal lamella that is nearly evenly narrowed toward the apex if viewed in dorsal aspect and almost straight if viewed laterally (Figs 43 View Figures 39–46 , 44 View Figures 39–46 versus 87, 89). Quasicalathus conservans sp. nov. differs from the above-described Q. agonicollis sp. nov. by larger body (SBL> 7 mm), less obtuse laterobasal pronotal angles, the more markedly concave elytral basal margin, more markedly projected humeri, the less obtuse humeral angle (<120°), and by the larger aedeagus.
Remarks.
Quasicalathus conservans sp. nov. and Q. elpis are, based on current knowledge, indistinguishable in their external characters but differ clearly in the shape and proportions of the male genitalia. Ball and Nègre (1972) and Schmidt (2018) detailed a similar situation found among many species pairs of Mexican and Himalayan Calathus that can only be separated by features of the male genitalia. We hypothesize that Q. elpis and Q. conservans sp. nov. were most likely allopatric species, distributed in geographically separated parts of the Eocene amber forests of northern Europe. Under this hypothesis, Q. elpis was endemic to the more western part of the Eocene forest and was thus fossilized in Baltic amber, while Q. conservans sp. nov. was endemic to the more eastern part of the area and therefore fossilized in Rovno amber. This assumption is consistent with the faunistic data showing that beetle fossils of Baltic and Rovno amber deposits have only few species in common (less than 13%; Matalin et al. 2021).
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