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, OCTOBER 2011, 62, 5, 463—475 doi: 10.2478/v10096-011-0033-8
Introduction
Chiapas amber is peculiar for its content of plant remains,
occasional fungi, scarce pulmonate gastropods, arachnids,
crustaceans, relatively abundant insects, amphibians, rep-
tiles, bird feathers and mammal hair (Poinar 2003; Engel
2004; Solórzano-Kraemer 2007; Vega et al. 2009a,b). In-
sects are represented by 235 species all of which belong to
146 living families and the living or closely related (n= 3)
genera. The termite Kalotermes nigritus Snyder, 1946
(Isoptera, Kalotermitidae), which still lives in South America
today (Zherikhin 1970) is famous.
It is worth mentioning that the earliest living insect species
are much older, originating from Eocene Baltic amber. These
species are Tetracha carolina (Linnaeus, 1766) (Coleoptera,
Cicindelidae), Colasposoma metallicum Clark, 1865; Palaeo-
mymar anomalum (Blood & Kryger, 1922) (Hymenoptera,
Mymaridae), Cupes tesselatus (Motschulsky, 1856) (Co-
leoptera, Cupedidae) and Setodes picescens Ulmer, 1912 (Tri-
choptera, Leptoceridae). Drosophila rubrostriata Becker,
1908 is known from the Oligocene of Fontainebleau.
The specimen reported here was collected from the Los
Pocitos locality (Fig. 1) of the amber-bearing Mazantic Shale,
Afro-Asian cockroach from Chiapas amber and the lost
Tertiary American entomofauna
PETER VRŠANSKÝ
1,2
, PAULINA CIFUENTES-RUIZ
3
, UBOMÍR VIDLIČKA
4,5
, FEDOR ČIAMPOR JR
4
and FRANCISCO J. VEGA
3
1
Geological Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P.O. BOX 106, 840 05 Bratislava, Slovak Republic;
geolvrsa@savba.sk
2
Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya 123, 117868 Moscow, Russia; lab@palaeoentomolog.ru
3
Instituto de Geología, UNAM, Ciudad Universitaria, Coyoacán, 04510 México D.F., Mexico; vegver@unam.mx
4
Institute of Zoology, Slovak Academy of Sciences, Dúbravská cesta 9, 845 06 Bratislava, Slovak Republic;
uzaevidl@savba.sk; f.ciampor@savba.sk
5
Department of Biology, Faculty of Education, Comenius University, Moskovská 3, 813 34 Bratislava, Slovak Republic;
vidlicka@fedu.uniba.sk
(Manuscript received January 28, 2011; accepted in revised form March 17, 2011)
Abstract: Cockroach genera with synanthropic species (Blattella, Ectobius, Supella, Periplaneta, Diploptera and ?Blatta),
as well as other insects such as honeybees, although natively limited to certain continents nowadays, had circumtropic
distribution in the past. The ease of their reintroduction into their former range suggests a post-Early Miocene environ-
mental stress which led to the extinction of cosmopolitan Tertiary entomofauna in the Americas, whilst in Eurasia,
Africa and Australia this fauna survived. This phenomenon is demonstrated here on a low diversity (10 spp.) living
cockroach genus Supella, which is peculiar for the circumtropical synanthropic brownbanded cockroach S. longipalpa
and also for its exclusively free-living cavicolous species restricted to Africa. S. (Nemosupella) miocenica sp. nov. from
the Miocene amber of Chiapas in Mexico is a sister species to the living S. mirabilis from the Lower Guinea forests and
adjacent savannas. The difference is restricted to the shape of the central macula on the pronotum, and size, which may
indicate the around-Miocene origin of the living, extremely polymorphic Supella species and possibly also the iso-
chronic invasion into the Americas. The species also has a number of characteristics of the Asian (and possibly also
Australian) uniform genus Allacta (falling within the generic variability of Supella) suggesting Supella is a direct
ancestor of the former. The present species is the first significant evidence for incomplete hiati between well defined
cockroach genera – a result of the extensive fossil record of the group. The reported specimen is covered by a mycelium
of a parasitic fungus Cordyceps or Entomophthora.
Key words: Mexico, synanthropic, fossil insects, parasitic fungi, Allacta, Supella miocenica sp. nov.
overlain by the Balumtum Sandstone (Fig. 1). Both lithostrati-
graphic bodies are regarded as informal units. The age of the
Chiapas amber has been a matter of debate. A Late Oligocene
to Early Miocene age has been proposed by Langenheim
(1966), Tomasini-Ortíz & Martínez-Hernández (1984), Santi-
ago-Blay & Poinar (1993), Bousfield & Poinar (1994), Poinar
& Brown (2002), Poinar (2003), Engel (2004), Castan
~eda-
Posadas & Cevallos-Ferriz (2007). Ferrusquía-Villafranca
(2006) described an artiodactyl from the Los Pocitos locality,
and considered a Late Oligocene age for these sediments,
based on previous biostratigraphic interpretations of Frost &
Langenheim (1974) and unreferenced paleomagnetic studies.
He suggested that the age of the Los Pocitos strata falls within
the 28—26 Ma (Ferrusquía-Villafranca 2006, p. 993). Other
authors suggest that the amber-bearing stratigraphic units are
of Middle Miocene age, and thus correlatives with the units
that produce amber in the Dominican Republic (Meneses-
Rocha 2001; Solórzano-Kraemer 2007; Solórzano-Kraemer
& Mohrig 2007; Perrilliat et al. 2010). At the Los Pocitos lo-
cality (Fig. 1), dark grey shales of the Mazantic Shale con-
tain amber, benthic foraminifera, gastropods, bivalves and
crustaceans. Based on
87
Sr/
86
Sr measurements taken from a
well-preserved shell of Turbinella maya from Los Pocitos,
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Vega et al. (2009a, p. 53) obtained an absolute age of 23 Ma
for the Mazantic Shale, placing it right on the boundary be-
tween the Oligocene and Miocene. The Mexican amber has
been interpreted as the resinous exudates of Hymenaea sp., a
leguminose tree whose communities developed near the an-
cient coast, in estuarine environments, very similar to man-
groves (Poinar 1992). It is worth mentioning, that the closest
relative of amber producing H. mexicana is the relictuous H.
verrucosa from East Africa (Poinar & Brown 2002). Another
amber species, H. allendis is a relative to H. courbaril of
Americas (Calvillo-Canadell et al. 2009). The amber was con-
sequently transported to a shallow marine environment (Lan-
genheim 1995; García-Villafuerte 2008).
The native representatives of the genus Supella are recent-
ly limited to Africa and are considered to have diverged ear-
ly in the phylogeny of the family, with the genus being the
second basalmost offshoot (after Nahublattella) of the Blat-
tellidae (Klass 1997). Nevertheless, their position is obscure
in some other analyses (see Ware et al. 2008), and there is a
single plesiomorphy recorded in respect to most Symploce
Hebard, 1916 (M and CuA longitudinal), which is consid-
ered to be the most primitive blattellid in our previous stud-
ies (Vršanský 1997). Thus Supella is most likely derived
from this genus (Vršanský et al. 2011) or its predecessors.
Thanks to the synanthropic Supella longipalpa Fabricius,
1798 (circumtropic – introduced by commerce), the mor-
phology of the present genus is well studied at the micro-
structural level (Roonwal & Rathore 1983). For example,
olfactory, gustatory, and mechanosensory receptors with a
density of 73.700 sensilla/mm
2
were found on the most dis-
tal segments of maxillary as well as labial palps (Prakash et
al. 1995).
The ecology of the genus is much less known. S. longipalpa
reproduces in temperatures between 25—33 °C (Tsai & Chi
2007). It can be a carrier of human intestinal parasites (Kinfu
& Erko 2008), Salmonella (Fathpour et al. 2003), perhaps a
cryptic species related to Gregarina blattarum von Siebold,
1839 (Clopton & Gold 1996) and an allergen source
(Tungtrongchitr et al. 2004). Its ootheca may often be parasit-
ized (over 19 %) by host-specific hymenopterans Comperia
merceti (Compere, 1938) (Encyrtidae) and Anastatus tenuipes
Bolivar & Pieltain, 1925 (Eupelmidae) (for details see
Narasimham 1992). Individuals infected by archiacanthoce-
phalan Moniliformis moniliformis (Bremser in Rudolphi
1819) spend more time in the shade (Moore & Gottelli 1992).
S. longipalpa nymphs may be more capable of producing
and utilizing extra metabolic water from food than Blattella
germanica (Linnaeus, 1767) nymphs (Melton 1995) and its
average motility and dispersion ability is also significantly
higher than those of B. germanica (Khrustalyova 1993).
The average life cycle takes 161 days.
The extremely close relation of the species described here
with the exclusively African S. mirabilis (Shelford, 1908) may
also be an indication of the possibility of living (at least mor-
pho-) species of cockroaches occurring in the Miocene. Living
cockroach species are still unknown in the fossil record, possi-
bly because of rapid phylogeny at their species level (Vršan-
ský 2008). Living genera of cockroaches (both primitive and
advanced) are known since the Eocene (Vršanský et al. 2011).
What is notable is the identity of the pronotum colouration
with numerous representatives of another unrelated genus
that includes synanthropic species, the genus Periplaneta of
the Blattidae, for example, circumtropical P. australasiae
(Fabricius, 1775). Additionally, Periplaneta such as P. indica
Karny, 1908 from China can be smaller (forewing length
16 mm) (Karny 1908) and superficially could be easily con-
fused with Nemosupella Rehn, 1947. Periplaneta is known
from Eurasia, starting from the Middle Eocene – P. eocaenica
Meunier, 1921, P. relicta Meunier, 1921 and possibly others
occur in Messel sediments (Schmied 2009). Miocene repre-
sentatives are P. hylecoeta Zhang, 1989 and P. lacera
Zhang, 1989 from the Shanwang and P. sphodra Zhang, Sun
& Zhou, 1994 from Shandong in China. P. houlberti Piton,
1940 is reported from the Late Oligocene of Menat in
France. The living genus and even some species have a cos-
mopolitan distribution. The origin of the synanthropic P.
americana is currently anticipated to have shifted to South,
Central and south of North America with the slave ships
from tropical Africa (Rehn 1945). Notably, both P. americana
and P. australasiae live both synanthropically and free
(Vidlička 2001). Supella can be easily discriminated from all
Periplaneta by the characteristic pale “band” and simplified
venation. The identical, but homoplastic habitus of cock-
roaches significantly differing in size (ca. 10 mm in amber
specimen; up to 30 mm in living Nemosupella and up to
60 mm in living Periplaneta) is obscure.
Another similar and related genus Allacta Saussure &
Zehntner, 1895 is really problematic, because the only signif-
icant difference of species placed in this genus is the geo-
graphical distribution which is limited to Asia, shape and
colouration of the pronotum and shape of subgenital plate.
The vast majority of characters are overlapping between Su-
pella and Allacta and most likely these two genera represent
Fig. 1. Location and stratigraphic column of the Los Pocitos locali-
ty of the Chiapas amber, Mexico.
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a single holophyletic taxon. Roth (1993) noticed the extreme
similarity of S. longipalpa and A. diluta. Nevertheless, al-
though we have studied all Allacta and Supella species, it is
not the aim of the present publication to revise both taxa. Be-
cause both, and especially Supella is extremely polymor-
phic, we retain the determination of the present species
within Supella and its subgenus Nemosupella, but it is evi-
dent Supella is a direct ancestor of Allacta.
The taxon is evidence of the rich cosmopolitan Tertiary
entomofauna, which went extinct in the Americas, but still
survives on other continents, in this case in Africa. The Afri-
can taxa apparently also gave birth to the rich but uniform
genus Allacta, radiated in the whole of Asia, and compara-
tively recently also in Australia. Allacta itself was also
present in America during the Eocene.
It follows that the horse was not the only group which
went extinct in the Americas, but could easily be reintro-
duced there by humans.
Material and methods
A single completely preserved specimen was collected by
Luis Zú±iga Miganjos in the Los Pocitos locality and is depos-
ited in Museo Comuntario del Ambar, Simojovel, Chiapas
(MUCAS, supported by Instituto Nacional de Antropología e
Historia – INAH). It was photographed using a Canon EOS
Mark II and drawn with a camera lucida from an Olympus
SZH10. Wing terminology follows Vršanský (1997). The liv-
ing undescribed Allacta or Supella sp. provided in Fig. 3 was
collected in Central Laos, Bolikhamsai province, Ban Nape-
Kaew Nua Pass [N 18°22.3
’/ E 105°09.1’], by Ondrej Šauša
and Eduard Jendek (deposited in IZ SAS Bratislava).
Parsimony analysis was performed using PAUP* software
version 4.0b10 (Swofford 2002), with a TBR heuristic search
of 1,000,000 replicates and the option ‘save multiple trees’ ac-
tivated. All characters were treated as unordered (0 – plesio-
morphic, 1, 2, 3 – apomorphic states). MaxTrees option was
set to 1000. Characters were weighted regarding their evolu-
tionary relevance (characters 9, 12 – weight = 10, character
13 – weigh = 1, remaining characters – weight = 5). De-
tails of the procedure of each character are explicitely stated
in the character analysis below. A heuristic search produced
1000 equally parsimonious trees with length 368 (consisten-
cy index CI= 0.29, retention index RI= 0.77). Majority con-
sensus tree was constructed and post-edited (coloured) in
MESQUITE software version 2.6. Only clades with frequency
> 50 % were retained.
Results
Systematic entomology
Order: Blattida Latreille, 1810 (= Blattaria Latreille,
1810 = Blattodea Brunner von Wattenwyl, 1882)
Family: Blattellidae Karny, 1908
Subfamily: Pseudophyllodromiinae Hebard, 1929
Supella Shelford, 1911
Fig. 2. Supella miocenica sp. nov. from the Miocene Chiapas amber of Mexico. Holotype MUCAS-001. a – Dorsal view; b – Ventral
view; c – Head; d – Fore leg; e – Fore tarsus. Original by PC and FV. Total specimen length (from the head to the end of wings) 10 mm.
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T y p e: Blatta longipalpa Fabricius, 1798 (circumtropical,
native in Africa).
= Blatta supellectilium (Serville, 1839)
= Blatta incisa (Walker, 1868)
= Ischnoptera quadriplaga (Walker, 1868)
= Blatta extenuata (Walker, 1868)
and numerous other synonyms of diverse specimens from the West
Indies (see Rehn 1947).
C o m p o s i t i o n: Besides the type; S. vicina Chopard,
1958 [Comores islands]; S. abbotti Rehn, 1947 [Kenya,
Tanzania, Malawi]; S. dimidiata Gerstaecker, 1869 [Kenya,
Congo, Angola, Rhodesia, Malawi, Mosambique, Botswana,
Natal, Transvaal]; S. orientalis Grandcolas, 1994 [Saudi
Arabia]; S. (Mombutia) chapini Rehn, 1947 [Congo]; S.
(Nemosupella) gemma Rehn, 1947 [Ghana]; S. (Nemosupella)
mirabilis [Cameroon, Gabon, Congo, Uganda, Kenya,
Tanzania]; S. (Nemosupella) occidentalis Princis, 1963
[Guinea]; S. (Nemosupella) tchadiana Roth, 1987 [Chad].
All extant in Africa.
D i a g n o s i s (Rehn 1947, in part): “Pronotum ovate sub-
trapezoideal in outline. Tegmina of female varying in length
from covering but half the abdomen to surpassing the abdomi-
nal apex by a distance equal to the pronotal length, in outline
ranging from 1.5 times as long as broad. Apex well-rounded.
Costal veins numerous, straight oblique, several of the more
distal ones usually ramose, reduced in number in the abbrevi-
ated tegmined forms; discoidal sectors oblique, tending to-
ward sublongitudinal in males of S. abbotti and S. mirabilis.
Anal field pyriform, anal veins five or more, regular; discoidal
sectors similarly developed, anal field always fully indicated.
Cephalic femora with ventro-cephalic margin bearing a
regular series of spines, evenly reducing in length and
strength distad (sometimes replaced by setae (e.g. in one
limb) – e.g. in S. mirabilis), apical spines of same margin
two-three in number, the terminal one much the longer; me-
dian and caudal femora with ventral margins spined; caudal
tarsi with metatarsus in length surpassing the other articles
combined. Arolia well developed; tarsal claw of equal
length, their margins unarmed, simple.”
Subgenus: Nemosupella Rehn, 1947
T y p e : Phyllodromia mirabilis Shelford, 1908.
C o m p o s i t i o n: Supella mirabilis, S. gemma, S. tchadi-
ana, S. occidentalis.
D i a g n o s i s (ex Rehn 1947 in part – only relevant
characters): “Females more robust with tegmina and wings
broader and in length less markedly surpassing the apex of
the abdomen, apex well rounded. Head pyriform in outline,
transverse facial ridge nearly straight transverse; palpi with
penultimate and antepenultimate articles elongate. Caudal
tarsi moderately slender, metatarsus in length somewhat ex-
ceeding that of the remaining tarsal articles combined”.
Supella (Nemosupella) miocenica sp. nov.
(Figs. 2a—c, 3a—c)
H o l o t y p e: MUCAS-001. A complete female.
T y p e l o c a l i t y: Los Pocitos, Simojovel de Allende,
Chiapas amber.
T y p e h o r i z o n: Lower Miocene, Mazantic Shale, Tertiary.
D i f f e r e n t i a l d i a g n o s i s: The present species differs
from its consubgeners, S. mirabilis in being smaller (total
body length with wings ca. 10 mm vs. 16—25.5 mm in S.
mirabilis), in having discoidal sectors oblique (oblique to
sublongitudinal in S. mirabilis), and in having the central dark
pronotal macula divided into two parts; from S. gemma in size
(similar as S. mirabilis), in having wings more coloured and
pronotal central macula smaller; from S. tchadiana of a com-
parable size (12 mm), in having pronotum without markings;
and from S. occidentalis in colouration and size.
D e s c r i p t i o n: Very small species (overall body length
without wings about 9 mm). Head small (length to width:
1.6/1.3 mm) with very fine antenna covered by a row (basal
segments) or up to four rows with four short (roughly corre-
sponding to segments’ width) sensilla chaetica in each.
Pronotum ovate subtrapezoidal in outline, significantly
vaulted (1.7/2.9 mm), pale, with dark macula covering the
whole posterior margin and central macula, divided into two
separate parts.
Body slender, sterna (especially the posteriormost ones)
widely carved, cerci with up to 16 segments, very long
(1.8 mm) with dense fine sensilla chaetica of diverse length
(0.2—2 times as long as the width of the median cercal seg-
ment). Legs slender, long (including fore legs), cursorial. Fore
legs terminated with claw and arolium; femora (1.7/0.1 mm)
with dense chaetica, tibia (0.9/0.07 mm) with at least 5 fine
spurs (arrangement of spines along the tibiae in 3 rows), tarsi
5-segmented (0.7, 0.2, 0.1, 0.05, 0.2 mm). Front femur Type
B2, with four proximal stout spines succeeded by a row of
uniform piliform spinules, terminating in two large spines;
pulvilli present only on the fourth tarsomere, tarsal claws sym-
metrical and unspecialized (simple), simple arolia present.
Mid femora wide and with numerous sensilla (about 26
spines in two rows) (2.1/0.6 mm), tibia also robust (1.6/
0.2 mm), with long fine spurs (10 or more); tarsi curious, ex-
tremely short (0.7/0.1 mm), with an indistinct claw and aroli-
um. Hind legs long, femora robust (2.6/0.8 mm), with two
rows with numerous (about 19 2) fine spurs and terminal two
fine spurs; tibia long (2.9/0.2 mm), with numerous (up to 30)
fine spines; tarsi long (1.3, 0.3, 0.1, 0.1, 0.3 mm), densely
haired, with distinct claw and arolium. First third of the first
Fig. 3. a—d – Supella miocenica sp. nov. from the Miocene Chiapas amber of Mexico. Holotype MUCAS-001. Ventral view. a – Com-
plete specimen with curculionid beetle; b – detail on head with mycelia of parasitic fungus Cordyceps or Entomophthora (white “bub-
bles”); c – detail on cercus; d – dorsal view, total specimen length (from the head to the end of wings) 10 mm. e – Undescribed male of
Allacta or Supella sp. from Central Laos. Total length ca. 12 mm. Nemosupella is even more similar in having the nearly identical pronotal
shape and colouration (the central macula is divided into 2 parts only in S. miocenica). Photograph of the sister species, S. (Nemosupella)
mirabilis is available free on the web (FOW).
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Fig. 3.
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tarsal segment sparsely (5) haired, the rest with at least 33 sen-
silla; second segment with 9, third with two, fourth with six
and terminal one with at least two sensilla.
Forewing dark, with characteristic pale anterior margins
and central stripe making the illusion of the body being sepa-
rated into two halves. Apex rounded. Venation simple, with
minimum deformities. Total number of veins meeting the
margin (without A) ca. 30. Sc simple, short, R nearly
straight, R branches simple except for the few terminal
branches (18 R veins meet margin). RS not clearly differenti-
ated. Discoidal sectors oblique. M secondarily branched,
with about 10 branches at the margin. CuA is fused with M
and perhaps consists of a single terminally dichotomized
branch. Anal field pyriform, fully indicated, anal veins sim-
ple, regular, apparently five or more. Intercalaries locally
distinct (in basal R and CuA) and probably common.
R e m a r k s: For comparison and details see Discussion.
Derivation of name: miocenica is after the Miocene epoch.
C h a r a c t e r a n a l y s i s: (0 – plesiomorphy; 1—3 – apo-
morphies relative to other species within genera Supella and
Allacta, and/or Cariblattoides Rehn & Hebard, 1927 and
Symploce (and fossil Piniblattella Vršanský, 1997), which
were chosen as outgroups based on high similarity, and
based on retension of all original states of characters due to
standard habitus (not derived like in Supella and Allacta):
1. Head with interocular (IO) space roughly identical with
the distance between antennal sockets: apomorphy; plesio-
morphic is partially reduced IO space (as in Symploce and
most regular cockroaches); IO space nearly absent is a strong
apomorphy (2), eyes very small and remote (3).
2. Pronotum large ovate subtrapezoidal in outline, signifi-
cantly vaulted: plesiomorphic (as in most cockroaches in-
cluding Symploce and Piniblattella); apomorphic states are
1) small and round; 2) subelliptical with margins parallel.
3. Pronotal colouration with basal dark stripe and two cen-
tral maculas: plesiomorphic (central maculas are present in
most primitive blattellids such as Piniblattella), derived states
are alternative colourations (dark with cental pale macula).
4. Subgenital plate long: apomorphy (plate is plesiomor-
phically of normal length in Symploce, Piniblattella and
most other blattellids).
5. Forewing with apex of radial area reduced to mostly
simple branches (RS indistinct): apomorphy (RS distinct in
primitive Symploce and Piniblattella).
6. Forewing M and CuA branched and curved: plesiomor-
phy (as in Mesozoic cockroaches); these branches are apo-
morphically longitudinal even in some Symploce; serrate (2).
7. Forewing colouration with characteristic transversal
stripes: apomorphy at level of common ancestor of Supella
and Allacta. Plesiomorphic state is colouration uniform but
not strong as in Cariblattoides, and other primitive blattel-
lids (Nahublattella, Neoblattella etc.).
8. Colouration of wings soft: plesiomorphy; pronotum
strongly dark, with sophistic pale stripes on forewing is apo-
morphic (funebris spp. group).
9. Colouration of wings and pronotum with continuous co-
louration: plesiomorphy; derived apomorphic state is colou-
ration in dark dots, lines and blotches. This character was
found as a global irreversive reorganization of morphology
and colouration and thus has been given higher weight in
the cladistic analysis.
10. Hindwing R1 distinct: plesiomorhy (as in most primi-
tive blattellids including Symploce and Piniblattella); R1 is
apomorphically reduced to a single vein.
11. Fore tarsi of B-type: apomorphy (tarsi are plesiomor-
phically A-type in most primitive blattelids including most
Symploce).
12. Pulvilli exclusively on 4
th
tarsomere: apomorphy (pulvilli
are plesiomorphically on 4 tarsomeres in primitive blattellids
including Symploce). In addition to diagnosis of Allacta (Saus-
sure & Zehntner, 1895), this character was found unique, never
occurring homoplastically in any other group (additionally un-
related with respect to size changes) and thus has been given
higher weight in the cladistic analysis.
13. 1 or 2 terminal fore femoral spurs: apomorphy (plesio-
morphic state is with 3 spines in both A- and B-types of
Symploce). This character was found polymorphic within
species and even on one specimen (L/R sides – Roth 1991,
1993, 1996 and our observation) and thus has been given
lower weight in the cladistic analysis.
14. Habitus robust: plesiomorphy (as in Piniblattella), de-
rived apomorphic states are slender (1), extremely fragile (2)
and extremely elongated (3).
Allacta Saussure & Zehntner, 1895
= Abrodiaeta Brunner von Wattenwyl, 1893
= Pseudochorisoblatta Bruijning, 1948
= Arublatta Bruijning, 1947
T y p e: Abrodiaeta modesta Brunner de Wattenwyl, 1893
from Carin Ghecu in Burma, by selection.
C o m p o s i t i o n: Funebris species group (sensu Roth
1993): basivittata (Bruijning, 1947) [New Guinea, Aroe and
Aru Islands], bipunctata (Walker, 1869) [Celebes, Aru Is-
lands, New Guinea], funebris (Walker, 1868) [Borneo] (Roth
1993); grandcolasi Roth, 1995 [Irian-Jaya], megamaculata
Roth, 1995 [Papua New Guinea], straatmani Roth, 1995
[Papua New Guinea] (Roth 1995), diagrammatica (Hanitsch,
1923) [Malacca, Singapore, Mentawai islands, Sumatra, Java].
Hamifera
species group (sensu Roth 1993): bimaculata
Bey-Bienko, 1969 [China], diluta (Saussure, 1863) [Ceylon,
India], figurata (Walker, 1871) [Ceylon, India], hamifera
(Walker, 1868) [Malacca, Java, Borneo, Philippinen], inter-
rupta (Hanitsch, 1925) [Borneo], luteomarginata (Hanitsch,
1923) [Singapore], maculicollis (Hanitsch, 1927) [Vietnam],
parva Shelford, 1906 [Borneo], pantherina (Hanitsch, 1933)
[Borneo] (Roth 1993); svensonorum Roth, 1995 [Malaysia,
Borneo] (Roth 1995).
Polygrapha
species group (sensu Roth 1993): fascia Roth,
1993 [Indonesia], immunda (Brunner von Wattenwyl, 1893)
[Burma, Malacca], polygrapha (Walker, 1868) [Thailand,
Malacca, Singapore, Sumatra, Borneo], picturata (Shelford,
1907) [Singapore, Sumatra, Thailand, Malaysia, Borneo],
marmorata Walker, 1869 [Burma, Sumatra, Malaysia],
mcgavini Roth, 1991b [Indonesia], robusta Bey-Bienko, 1969
[China], transversa Bey-Bienko, 1969 [Vietnam]; arborifera
(Walker, 1868) [Malaysia, Java, Borneo, Mentawai Islands],
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Cariblattoides with A-type and pulvilli on 4 tarsomeres, sup-
porting this state as ancestral.
Phylogenetically obscure is also the distribution of knee
spines at the distal end of the femora – 2 in present species
and some Allacta (see character matrix) and Supella, but more
often 3 (also in figured most closely related Allacta sp.).
The present amber species clearly differs from representa-
tives of the A. funebris species group, which are very dark
including the pronotum (eventually with a narrow pale mar-
gin only) and with basal narrow pale stripes. A. polygrapha
spp. group differs in having a large symmetrical pronotal
pattern of dark dots, lines and blotches and forewings che-
quered with dark cells between veinlets and with larger
blotches (A. confluens placed here is somewhat different
from other representatives of this species group, it has more
coherent colouration and pronotum colouration most similar
to the amber specimen. Nevertheless, the shape of the prono-
tum of S. miocenica is different: dissimilar to any described
Allacta spp.). A. puncticollis is also completely different,
with a subparabolic reddish brown pronotum with small yel-
lowish spots, but has pulvilli limited to the 4
th
tarsomere. A.
crassivenosa is categorized as incertae sedis and most likely
belongs to another genus. The most related to the present
amber species within Allacta is the A. hamifera spp. group,
which differs in having smaller pronota with a different colou-
ration pattern and in the shape of the subgenital plate which is
never as long in Allacta. Even more similar, and hardly recog-
nizable from the Nemosupella spp. is an undescribed represen-
tative putatively attributed to Allacta on the basis of identical
legs (pulvilli limited to the 4
th
tarsomere – Figure 2b). Alter-
natively it can mean that this species belongs to Supella and
is its only Asian representative, but more likely it is a transi-
tional taxon leading to Allacta. The figured undescribed spe-
cies (Fig. 3e) cannot be placed into any spp. groups of
Allacta, but is most closely related to the A. hamifera spp.
group in the shape of the head and underived colouration. It
is apparent that A. funebris and A. polygrapha spp. groups
were derived much later, the latter apparently derived via A.
confluens, which has similar pronotum colouration and un-
derived forewing colouration.
It is clear, that there is no strict hiatus between these two
genera, but this cannot be used as a reason for their synony-
mization or for the erection of additional genera. The problem
is that there are known “missing link” taxa in all cockroach
families and we also know a half-cockroach—half termite
(Vršanský 2010) and also half-cockroach—half mantodean. All
studied living cockroach genera with fossil records have these
transitional stages too, and the present taxon is no exception.
This is a half-Supella—half-Allacta, but better Supella than
Allacta. So splitting or erecting does not have a proper place
here just because the group is well studied. Paraphyletic taxa
and incomplete hiati are present in the vast majority of studied
cockroaches, which is a result of the extensive fossil record
with ca. 100,000 specimens. So our specimen has synapomor-
phies of Allacta+Supella (colouration, venation), autapomor-
phies of Allacta (extremities), but major autapomorphies of
Supella (pronotum, subgenital plate).
The cladogram (Fig. 4) supports all the above-mentioned in-
ferences, with nearly ideal separation of all spp. groups, but it
australiensis Roth, 1991 [Queensland], confluens (Hanitsch,
1925) [Borneo], labyrinthica (Hanitsch, 1927) [Vietnam],
loconti Roth, 1993 [Indonesia], megaspila (Walker, 1868)
[Malacca, Mentawai Islands, Java, Borneo], ornata Bey-Bien-
ko, 1969 [China], modesta (Brunner von Wattenwyl, 1893)
[Burma; type], karnyi (Hanitsch, 1928) [Mentawai Islands,
Sumatra] (Roth 1993), brossuti Roth, 1995 [Irian-Jaya],
deleportei Roth, 1995 [Papua New Guinea], gautieri Roth,
1995 [Papua New Guinea], nalepae Roth, 1995 [Papua New
Guinea], persoonsi Roth, 1995 [Papua New Guinea], srengi
Roth, 1995 [Papua New Guinea] (Roth 1995).
A. puncticollis (Brunner von Wattenwyl, 1898) [Borneo]
(not placed sensu Roth 1993) and A. crassivenosa Bolívar,
1897 [India] (incertae sedis sensu Roth 1993). Except for
problematic A. australiensis, all are extant in Asia.
D i a g n o s i s: Front femur Type B [B2 or B3 according to
Roth 1993, or C (right and left femur can differ in type (B2-B3
or even B-C) according to Roth (1991, 1996))]; pulvilli
present on fourth tarsomere only, tarsal claws simple, sym-
metrical, arolia present (Roth 1995).
Discussion
Supella-Allacta complex
Because there is an immense similarity and relation be-
tween the genera Supella and Allacta, it is necessary to pro-
vide arguments for the categorization of the present fossil
within Supella.
These genera are clearly distinguished among other blat-
tellids by autapomorphies including the characteristic colou-
ration with a pale stripe appearing to divide the body into
two (or, in combination with the pronotal colouration into 3)
separate parts; M and CuA descending in an obtuse angle;
mostly simple R branches with indistinct RS (homoplastic
with Pseudomops Serville, 1831 and Ectobius Stephens,
1835); and in other characters unseen in the present fossil (see
Rehn 1947). Supella restricted to Africa is much more diverse
and polymorphic (including forms identical with Allacta)
which suggests its direct ancestral position in respect to
Asian and Australian Allacta (the latter is restricted to
a single species A. australiensis from Queensland, which has
an indicated hindwing R1 as in Supella, but is very different
from both Supella and Allacta in having eyes nearly con-
nected, and in subelliptical – with anterior and posterior
margins parallel – form of pronotum; thus it can simply
represent Supella or a different genus).
The present amber species has fore legs of B type identical
(!including the number of proximal spines and terminal
spurs) with Allacta, dissimilar to most Supella (A-type), but
these types can be polymorphic (L/R) in a single specimen
of Allacta (B2/B3 or even B/C – see above), and the Supella
subgenus Nemosupella can have this B-type pattern too. The
most primitive living blattellid, Symploce has mostly A3
type, but ocassionally B3, thus it is likely A is the original
type, but the above-mentioned polymorphisms are evidence
for a convergent nature of this character changes. Closely re-
lated and perhaps derived from Supella is also the genus
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was weak in the position of A. interrupta (well nested within
hamifera group by intuition (Roth 1993), very closely related
to A. hamifera) within the polygrapha group. The second prob-
lem is the terminal position of A. confluens which is expected to
be the basalmost polygrapha group stem (it has a very basal
position when all characters were equally weighted). Third, A.
bimaculata+A. pantherina (hamifera spp. group) appear nest-
ed within Supella. Notably, all three problems are absent in the
cladogram with the normal weight of character 13 (weight 1 in
contrast to weight 5 of all other characters except weight 10 of
characters 9 and 12), which is polymorphic (and thus has been
given a lower weight), A. bimaculata + A. pantherina (hamifera
spp. group) are nested (as basalmost offshots) within hamifera
spp. group using the same weights but using different (500)
number of maximal search trees. A. puncticollis (out of any spp.
group) appears to be a sister taxon to A. svensonorum and A. lu-
teomarginata (trichotomy at cladogram). When all characters
were weighted normally and in many other options tried, S. di-
midiata were often nested within Allacta. S. dimidiata is a good
Supella, and this placement is evidence for numerous homopla-
sies within the group. Generally, the homoplasies wihin cock-
roaches are enormous.
Paleogeographically, the basalmost blattellids were pre-
served in Asia, but their ancestors within the Mesoblat-
tinidae were also common in Europe (Vršanský & Ansorge
2007). The basalmost Supella is up to recently clearly nested
within Africa, but the present American species is clear evi-
dence for the past circumtropic distribution. Allacta was pos-
sibly derived in Africa but radiation was apparently not
limited to Asia (except for the mentioned synanthrope, Al-
lacta is present in sediments of the Green River in Colo-
rado). According to this cladogram A. australiensis was
derived quite recently from one of the species in the
polygrapha spp. group.
From the most primitive blattellids, Nahublattella and
Symploce (for position of these genera within Blattellidae
see also Klass & Meyer (2006)), there is a significant reduc-
tion and simplification of venation, which is evidence of the
very early divergence of the whole complex from the main
blattellid stem. Another eventual conclusion considers the
small size of the present species, which may be a plesiomor-
phic character, which would explain the significant simplifi-
cation of venation even in large living species. Notably, in
the derived genus Allacta, terminal radial veins are simpli-
fied only in the smallest species (A. parva).
Notwithstanding, some living Supella and Nemosupella in
particular have more primitive traits and likely diverged be-
fore the speciation of S. miocenica. Its single insignificant
deformity (not clearly visible, insignificantly changing the
wing geometry) supports the fact that Eocene and Miocene
species have few accumulated wing deformities and their oc-
currence in living species represents support for them being
inheritable mutations (see Vršanský 2005).
Extinct American
Supella
In spite of the close relation of its 3 known subgenera, the
general habitus of the respective taxa in Supella is very di-
verse. S. longipalpa is a slender, fine cockroach, while S.
orientalis has extremely elongated wings (—1 : 4.5), and the
subgenus Nemosupella is clearly differentiated by robust
habitus with a robust unplain pronotum and more or less nor-
mal longitudinal veins. The present species share all the au-
tapomorhies of the genus and subgenus Nemosupella and
can be safely categorized within this taxon.
The colouration and general appearance is hardly recog-
nizable from females of S. mirabilis, its sister species, al-
though the shape of the pronotum is somewhat transitional
between its males and females. Except for the significantly
smaller size of the present new species, the sole difference
between the two taxa is the divided central pronotal macula.
There are no additional plesiomorphies, which indicate the
present as well as the living species of Nemosupella diverged
near the Mid-Miocene. The other three representatives of the
subgenus are closely related to S. mirabilis, but are dissimi-
lar to the present fossil due to different colouration.
On the other hand, other representatives of the genus such
as S. longipalpa reveal significant divergence from the main
morphological standard and suggest rapid phylogeny at the
subgeneric level.
The similarity with the undescribed representatives of the
genus Allacta (Fig. 3e) is so striking (and involves size – Ne-
mosupella are much larger), that it is apparent Allacta is de-
rived from Nemosupella via the predecessors of this
undescribed taxon and also via predecessors of Supella mio-
cenica. Its direct ancestry can be excluded based on the de-
rived pronotum of S. miocenica. While there is a standard
Allacta placed within a living spp. group (polygrapha)
present in much older Eocene Green River sediments, the
Chiapas is apparently another case of the presence of primitive
species in amber, when compared to isochronous sedimentary
record. Relic character of amber cockroach (and all insect to
some extent) assemblages is characteristic also for the only
two studied Mesozoic ambers (Lebanon and Archingeay, but
also in Baltic amber), which might either be caused by dif-
ferent methods of dating, or by the more humid, dark and
colder source microclimates of amber forests. This is in con-
trast to Cretaceous ecosystems, where primitive cockroach
forms of the Jurassic type are restricted to younger, but dry
to semiarid ecosystems (Vršanský et al. 2002).
Very little can be said about the ecology of the present spe-
cies. Generally the ecosystems of Chiapas were perhaps di-
verse, ranging from lowland tropical dry forest tending toward
open forest and mangroves (Solórzano-Kraemer 2007). The
wide range of ecosystems from the rainforest down to savan-
nas, of the closely related S. mirabilis, indicate this genus is
highly adaptable to diverse conditions. This ecological plastic-
ity could have resulted in invasions of early Supella (Nemosu-
pella) into the Americas before the Mid-Miocene (and later
into Asia as the genus Allacta). Living species of Supella are
cavicolous (Grandcolas 1994) and the genus most likely also
originated in Africa because the most primitive blattellid, Sym-
ploce Hebard, 1916 is circumtropic, but rare in America. On the
other hand, the genus Nahublattella Bruijning, 1959 considered
to be even more primitive by Klass (1997) is native to Central
and South America, which could indicate the opposite.
The parasitic (or predatory) fungus Entomophthora or
Cordyceps is indeterminable, but the mycelium is richest in
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Fig. 4. Parsimony analysis of all the known Supella and Allacta species (excluding obscure A. crassivenosa, S. occidentalis, S. vicina, and
including 3 undescribed Allacta and/or Supella species) with their geographic distribution. S. miocenica and Piniblattella vitimica are ex-
tinct. Position of A. interrupta (top) is illusory due to numerous homoplasies with A. robusta and other polygrapha spp. group species, as
this species apparently belongs to the hamifera spp. group. 50% majority consensus tree from 1000 equally parsimonious trees was gained
with maximum parsimony search (PAUP). Numbers above branches represent clade frequencies in %.
the junction of head and pronotum and could have its epicen-
tre in the head. This fungus provides a contribution to the
poorly known microorganisms of the Chiapas amber. Only a
?Bacillus-like cell and two types of budding-bacteria-like
microrganisms were reported previously (Veiga-Crespo et
al. 2007).
Comments on synanthropism in cockroaches
The fifty species of synanthropic cockroaches comprise
only an insignificant fraction of the total of about 5000 (Bell
et al. 2007) described species of living cockroaches. Neverthe-
less, they are important for their number and ecological signif-
icance. Most of the species had their genera recently limited to
certain continents and only nowadays have become cosmopol-
itan (or circumtropical). On the contrary, their history on a
geological scale is much richer than we would expect and
their original distribution was also circumtropical.
The genus Blattella was until very recently limited to Africa
(26 species), Asia and the Pacific islands (23 species) (Roth
1985), and the synanthropic species B. germanica spread to
the whole world from east Asia (Roth 1985). The occurrence
of this genus in the Mesozoic of Europe as a single nymph
(adult could eventually differ) (Vršanský 2008) and in the
Eocene of the USA (Green River, Colorado) is thus surprising.
Free Ectobius is limited to Europe, but in the Tertiary it was
cosmopolitan. The same situation is found with the present
Supella introduced from North Africa to Central America on
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slave ships (Rehn 1947). The Miocene of Mexico is quite dis-
tant from the recent distribution limited to Africa.
According to Princis (1954), Blatta originates from the
Near and Middle East – the native place of the closely relat-
ed Shelfordella Adelung, 1910, but the other predicted origin
of this genus is North Africa (Rehn 1945; Cornwell 1968),
and Blatta furcata Bohn, 1985 is known from the Near East
and North Africa (Bohn 1985). Their close relative also oc-
curred in the Eocene of the USA (Green River).
The last significant synanthrop is Periplaneta, recently
limited to Asia.
The only viviparous cockroach group met the same fate:
the Diplopteridae, now restricted to two genera (one African,
one Asiatic), were common in America during the Eocene
(in Green River). This family is also reported from the
Eocene of Quilchena (Archibald & Methewes 2000), but the
figured specimen (Q-0040) is very different from all known
Diplopteridae (details to be provided elsewhere).
Thus it is apparent that all the synanthropic species belong
to cosmopolitan genera (cosmopolitan genera are otherwise
rare), very likely with a broad environmental tolerance – and
thus pre-adapted for synanthropism.
Lost Tertiary American entomofauna
The occurrence of some cosmopolitan synanthropic spe-
cies in the Americas and their absence prior to re-introduc-
tion, triggered the present discussions about the causes of the
extinction of these entomofaunas during the Tertiary.
It was Eocene Ectobius from the Green River – a member
of an extinct genus, but which was extremely easily reintro-
duced in North America several times (with 3 species),
which concentrated our efforts on the search for this fauna in
2006. It was very rapidly supported by the discovery of a
honey bee in the Miocene sediments of Nevada (Engel et al.
2009), a genus extinct in the Americas.
Poinar et al. (1999) also noticed the Early Tertiary North
American extinctions of species of living tropical ant genera
Technomyrmex Mayr, 1872, Leptothorax Mayr, 1855 and
Dolichoderus Lund, 1831, recorded in the Eocene of British
Columbia. These records comprise only the species level,
which is insignificant on the present time scale, but Techno-
myrmex is now, with the exception of a single Central Amer-
ican species (and its abundance in the Dominican amber),
limited to the tropics of the old world; Leptothorax is holarc-
tic today; Dolichoderus is cosmopolitan.
The Eocene of the Okanagan Highlands reveals a represen-
tative of the Myrmeciinae, currently limited to the Australian
region (Archibald et al. 2006). The only genus – determined
hemipteran from Quilchena, Megymenum is today found in
only in the Oriental biotic region and Australia (G. Gross,
personal communication in Archibald & Mathewes 2000).
The post-Miocene cooling was unlikely to be a reason for
this extinction, as both Ectobius and Apis Linnaeus, 1758
occur in Northern Europe today.
The loss of another taxon from North America is now ap-
parent – Supella, in which case cooling could be the reason
as nowadays this genus is restricted to Africa. On the other
hand it is hardly possible that this taxon went extinct in
warm Central and South America. Their historical absence in
South America is also difficult to anticipate as other cock-
roach taxa from the Dominican amber are present in South
America (see below).
Thus, of fourteen studied cockroach genera (all still living)
from the Eocene—Miocene of North America only two (Cari-
blattoides, Sigmella) survive nowadays in (South and Central)
America and only Cariblattoides is characteristic for Central
America (although it occurs in Brazil). It is perhaps not inci-
dental that a representative of Sigmella was dominant during
the Eocene and also in the present Mexican amber. An addi-
tional taxon reported from the Mexican amber is Ischnoptera
sp., currently distributed in Central and South America, but
this determination is obscure (determination may be correct,
but no diagnostic characteristics for the genus are provided,
and the species (Ischnoptera sp. 1 in Solórzano-Kraemer
2007) may well belong to Supella or some other blattellid
taxon). All things being equal, the diversity of cockroaches in
Chiapas amber was certainly high: 7 specimens belong to
7 different genera and species of the family Blattellidae.
Another cockroach genus, exclusively African today,
known from the Tertiary of North America is Namablatta
Rehn, 1937.
The closely related termites are ubiquitous in the present
context. While Kalotermes nigritus still lives in South Amer-
ica, the whole cosmopolitan family Mastotermitidae (present
as Mastotermes electromexicus Krishna & Emerson, 1983
and Mastotermes electrodominicus Krishna & Grimaldi,
1991 occurring in the Dominican amber according to Solór-
zano-Kraemer (2007)) went extinct in the Americas and sur-
vives only in Australia.
Some other insect groups from the Mexican amber (Solór-
zano-Kraemer 2007) and Green River (our data) reveal a
similar pattern, to be analysed in detail elsewhere.
It is of special consideration that the Dominican amber
shows a very different pattern in respect to the distribution of
cockroach genera. If the determinations of Arillo & Ortun
~o
(2005) are correct, then there are no shared taxa (even on the
generic level) between the Mexican and the Dominican am-
ber, and all Dominican amber cockroach genera are not only
highly advanced, but with the exception of the circumtropical
Anaplecta Burmeister, 1838 all – Euthlastoblatta Hebard,
1917, Pseudosymploce Rehn & Hebard, 1927, Plectoptera
Saussure, 1864, Cariblatta Hebard, 1916, Holocompsa Bur-
meister, 1838 (a single species (H. debilis (Walker, 1868))
also occurs in Ceylon, Java, Sumatra, Borneo and Phil-
lipines) – are characteristic of Central and/or South America.
Taxa described by Gorochov (2007), including obscure
Agrabtoblatta Gorochov, 2007 and Erucoblatta Gorochov &
Anisyutkin, 2007, also appear limited to South America.
Taking all this preliminary information together, it is ap-
parent that sometime after the Mid-Miocene some extensive
environmental change influenced North and probably also
Central and South America, resulting in the loss of cosmo-
politan Early Tertiary entomofaunas. Judging from the mod-
ern composition of the Dominican amber, this may (if the
abovementioned determinations are correct) mean a recovery
occurred during the time between the Early Miocene Mexi-
can amber (23—7.1 Ma) and the Dominican amber times
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(20.5—16.4 Ma). The dating of both of ambers is still uncer-
tain (the abovementioned datings are after EDNA database),
more counterbalanced by the Late Barstovian (14.5—14 Ma)
dating of the Nevada (with honeybee) sediments. Recently,
the age of 23 Ma was designated for the basalmost amber
bearing strata of Chiapas (Vega et al. 2009a).
As it is very difficult to imagine some geological or eco-
logical process which would be able to trigger such an exten-
sive change (aridization and/or cooling would not influence
some of the cockroaches), the change was probably biologi-
cal – either caused by diversification of cockroach parasites
which were consequently reduced (as reintroduction has
been easy), or diversification of more progressive insect
groups. The parasite hypothesis may be valid in the present
case, as Comperia merceti eradicated populations of synan-
thropic cockroaches in Europe, even when its function as a
control of Supella is still not validated (Goudey-Perriere
1991) and Encyrtidae and Eupelmidae parasitizing ootheca
have Tertiary origin (A.P. Rasnitsyn, personal communica-
tion 2010), known only from Europe starting with the
Eocene Baltic amber (Trjapitzin 1963). (These parasites
could also cause extinctions of external ovipositor bearing
cockroaches which did not lay eggs in ootheca.)
The occurrence of advanced taxa in the Dominican amber
(isochronous with the Mexican amber according to Solórza-
no-Kraemer (2007), however see above) would favour the
diversification and radiation of the modern South-American
cockroach taxa hypothesis. Nevertheless, Diploptera is the
most advanced cockroach that has ever lived, and thus its ex-
tinction in the Americas falsifies the latter hypothesis. On
the other hand, it is possible that its viviparity evolved only
in the common ancestor of Asian and African species.
Plants were perhaps not as influenced as fauna, as Eocene
flora of British Columbia in Canada is characteristic of the
modern eastern North American deciduous forest zone, prin-
cipally the mixed mesophytic forest, but also including ex-
tinct taxa: taxa known only from eastern Asian mesothermal
forests, and a small number of taxa restricted to the present-
day North American west coast coniferous biome (Green-
wood et al. 2005). Also, according to Solórzano-Kraemer
(2007), all plants from the Chiapas amber are currently
present in Pacific coastal forest.
Conclusions
The genus Supella with S. miocenica sp. nov. was native to
America during the Miocene time of the Chiapas amber. It
represents another case of rich cosmopolitan Early Tertiary
entomofauna, which suddenly went extinct in America some-
where around the Miocene (but which still survives in other
continents). Supella/Allacta complex (Allacta was derived
from Supella) is another case of the genera which now in-
cludes synanthropic species, which were natively circumtrop-
ic, and can be easily reintroduced in America nowadays. S.
(Nemosupella) miocenica sp. nov. is the earliest known cock-
roach which can be categorized within the living subgenus
and also the first published direct evidence of transitional spe-
cies (and thus incomplete hiatus) at the level of living genera.
Acknowledgments: We thank the Museo Comunitario del
Ámbar de Simojovel, Chiapas for making this material avail-
able for study; the generous support of Luis Zún
~iga and Jorge
Balcázar is greatly appreciated; Sonia Fraga Lopes (National
Musem, Rio de Janeiro), Dong Ren (Capital Normal Universi-
ty, Beijing), Maria del Carmen Perrilliat (Institute of Geology,
Mexico), Jozef Michalík (Geological Institute, Slovak Repub-
lic) and five anonymous reviewers for revision of the manu-
script, Ladislav Roller (Institute of Zoology SAS, Bratislava)
for literature supply, Ivona Kautmanová (Slovak National
Museum, Bratislava) for fungus determination and Graeme
Butler (Bratislava) for linguistic correction. Supported by the
UNESCO, AMBA/NUUR, VEGA 6002, 2/0125/09, 2/0167/9,
MVTS and the Literary Fund.
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