New taxa of extant and fossil primitive moths in South-East Asia and their biogeographic significance (Lepidoptera, Micropterigidae, Agathiphagidae, Lophocoronidae)

We report some surprising recent distributional range extensions of one extant genus and two more families of primitive moths discovered in amber fossils from South-east Asia which were previously only known from Australia and/or the southwestern Pacific, with the possible exception of an undescribed Siberian fossil attributed to Lophocoronidae. During entomological field work in rain forests of central Vietnam a new species of Micropterigidae was discovered. It is described herein as Aureopterix bachmaensis sp. nov. based on male and female specimens collected at light in the Bach-Ma National Park. The identification was corroborated by a molecular analysis. This is the first record of this genus in the Northern Hemisphere, previously thought to be restricted to the Australian Region (including New Caledonia). First results of investigations of Burmese amber inclusions now reveal the presence of the Australian Region families Agathiphagidae and Lophocoronidae in the Cretaceous of Asia. The fossil taxon Agathiphagama perdita gen. nov., sp. nov. is established on the basis of two females and this is assigned to Agathiphagidae. The fossil genus Acanthocorona gen. nov. is established in Lophocoronidae and includes seven species described here as A. skalskii sp. nov., A. bowangi sp. nov., A. muelleri sp. nov., A. kuranishii sp. nov., A. sattleri sp. nov., A. spinifera sp. nov. and A. wichardi sp. nov. The new species can be distinguished by the male genitalia which are illustrated together with wing venation and other morphological characters. The disjunct ranges of these taxa are discussed in a historical biogeographic context. Vicariance and dispersal hypotheses explaining the disjunct pattern are discussed. The discovery of these new species suggests a broader ancestral range of Aureopterix, Agathiphagidae and Lophocoronidae. Their extant ranges may be regarded as remnants or relicts of a wider distribution in the Mesozoic, or at least in the case of Aureopterix they could be the results of recent or ancient dispersal processes, since the calibration of molecular splits does not so far accord with plate tectonics.


Introduction
In continental South-East Asia the faunas of the Eastern Palaearctic and Oriental Regions share a common border. This borderline is not a clear-cut delimitation and separation of both faunas, but rather a broad transition zone extending from the slopes of the southern Himalayas in northern India to northern Myanmar, Thailand, Laos, Vietnam and southern China including Taiwan (Müller 1981).
This zone includes biodiversity hotspots for many insect groups (Balian et al. 2008;Konstantinov et al. 2009) and is also seen as a diversity centre of vascular plants ( Barthlott et al. 1999). It does not simply combine taxa from different biomes, but is also home of a great number of endemic species. The existence of these species might be evidence of an enduring ecological stability and favourable conditions facilitating both the evolution of recent neo-endemics and the persistence of older palaeoendemics (Fjeldså and Lovett 1997). Taxa belonging to old lineages dating back to the Mesozoic are of particular interest. In Lepidoptera, the following genera of homoneurous families, which represent these lineages, were documented with autochthonous species occurring in the area to date (Meyrick 1909;Issiki 1931;Issiki and Stringer 1932;Hwang 1965;Mutuura 1971;Davis et al. 1995;Mey 1997;Hashimoto and Mey 2000;Chen et al. 2009;Hirowatari et al. 2009;Lees et al. 2010): Micropterigidae: Micropterix Hübner, 1825, Paramartyria Issiki, 1931, Vietomartyria Hashimoto & Mey, 2000Eriocraniidae: Eriocrania Zeller, 1850 Hepialoidea: Ogygioses Issiki & Stringer, 1932Neopseustidae: Neopseustis Meyrick, 1909, Nematocentropus Hwang, 1965 A common feature of primitive moths is the low number of collected specimens for the majority of species. The species are rarely encountered in nature, and almost every new record merits communication. The scarcity of hitherto found specimens, however, suggests the occurrence of further relict species. Concerning Microlepidoptera, continental South East Asia has not been sufficiently explored, and new discoveries remain to be made, particularly in the mountain ranges of the Palaearctic-Oriental transition zone.
During the first field trip of the joint Vietnamese-German project VIETBIO to Central Vietnam in 2018, the first author was searching for caddisflies and micromoths in the Bach-Ma National Park (Mey et al. 2020). A single micropterigid female was collected at lights on 10.06.2018. Intensive searching at the locality for additional specimens yielded no results. Two days later, collecting in a different valley of the National Park, the corresponding male was found, again at the lights. Previous records of Micropterigidae were restricted to the north of Vietnam (Mey 1997), and the family was not expected to occur in the south.
Closer inspections of the specimens identified them as belonging to Aureopterix Gibbs, 2010, a genus reported so far only from Australia and New Caledonia (Gibbs 2010). Though similar in morphology to the two hitherto described species, the Vietnamese specimens represent a new, distinct species for this genus, which is described herein.
Examination of insect inclusions in Burmese amber resulted in the discovery of individuals which were identified as putative species of Agathiphagidae and Lophocoronidae. Both families are currently regarded as extant, endemic families of Australia and Southwest Pacific Islands. Interestingly, Skalski (1979) has tentatively determined a fossil individual from Siberian amber (Tajmyr region) of Upper Cretaceous (Santonian) as a representative of Lophocoronidae. The species was, however, not formally described and named. Burmese amber originates predominantly from the Hukawng Valley near Myitkyina, Kachin State, Myanmar (Fig. 1). It derives from an amber-bearing layer, which is not exposed at the surface but extends to a depth of 2-15 m (Cruickshank and Ko 2003). The amber deposits have been dated in detail by Shi et al. (2012). The age determination is of early Cenomanian (98.8 ± 0.6 Ma) given by U-Pb dating of zircons from the volcanoclastic matrix of the amber (Shi et al. 2012). The first synopsis of identified biota from Burmese amber was published by Grimaldi et al. (2002). A regularly updated catalogue of described taxa is available online (Ross 2019). There are only a few species of Lepidoptera described from this class of amber (Sohn et al. 2012). Representatives of the family Micropterigidae were encountered quite often in inclusions, and therefore, led to the descriptions of five species (Zhang et al. 2017;Cockerell 1919) which were assigned to the extant genus Sabatinca (Walker, 1863). One species was described in Douglasiidae, a placement (Poinar 2019a) that needs to be confirmed. These are the only available descriptions of Burmese amber Lepidoptera. The Burmese amber, however, contains a diverse and rich fauna of Microlepidoptera of ancient and more derived forms, which are currently under investigation and documentation (see Mey 2019). The following descriptions are some first results and are included in this article for providing a biogeographical context in the discussion on the unexpected discovery of Aureopterix bachmaensis sp. nov. in Vietnam.

Extant taxa
The adult moths were pinned and set in the field. Genitalia drawings were performed prior to embedding in Euparal on a genitalia slide. A camera lucida attached to a Leica MZ12 compound microscope was used. Genital preparations were made according to the procedure described in Robinson (1976). The genitalia were embedded in Euparal. Chlorazol Black was used to stain the membranous parts of the genitalia. Photographic documentation of imagines was done with a Leica Z 16 APOA Microscope in combination with a Leica DFC490 camera and Leica Application Suite programme, version 4.5.0 on a Windows PC. The map ( Fig. 1) was produced with ArcGIS software.
DNA extraction and sequencing DNA extraction were performed with a NucleoSpin Tissue kit (Macherey-Nagel, Düren, Germany). The standard forward and reverse primers LCO/Nancy for the DNA barcode region failed at amplifying the target region. The COI barcode was thus amplified in two parts refered to as COI fragment 1a and 1b, using primers from Léger et al. (2020). PCR-mix consisted of 17.8 µl ddH 2 O, 2.5 µl 10× Puffer, 1 µl Mg (25 mM), 0.5 µl dNTP Mix, 0.5 µl of each primer, 0.2 µl of Taq polymerase (New England Biolabs, Ipswich, USA) and 2 µl of the DNA sample, totalling a volume of 25 µl. PCR program was that of Léger et al. (2020). PCR product cleaning and sequencing were performed by MACROGEN (Netherlands).

Sequence analysis
Sequences were eye-checked under PhyDE 0.9971 (Müller et al. 2005), also aligned visually with other DNA barcode sequences of Aureopterix and Sabatinca retrieved from BOLD (http:// v4.boldsystems.org/). Phylogenetic analyses were performed on RAxML on the CIPRES portal (Miller et al. 2010), with Rapid Bootstrap Search stopped after 252 replicates. K2P distances were calculated on MEGA X (Kumar et al. 2018).

Fossil taxa
Photos of fossil species were taken using a Leica stereomicroscope M 420 Apozoom in combination with a Canon EOS 80D, EOS utility software and the Zerene Stacker software.
The fossils were examined under incident and transmitted light using a stereomicroscope (Leica MZ125). Line drawings were produced with a Leica camera lucida and digitally processed using Adobe Photoshop CS4. Measurements were made with the ocular micrometer of the stereomicroscope.
The terminology of genitalia structures used in the descriptions of taxa follows Gibbs (2010) for Micropterigidae, Kristensen (1998) for Agathiphagidae and Nielsen and Kristensen (1996) for Lophocoronidae. For each of these families a separate superfamily taxon was established (see Kristensen and Skalski 1998). The use of these names was found to be dispensable here, because they provide no additional information for the families and the taxonomic contents of the present article. Etymology. The specific name is derived from the name of the Bach-Ma National Park. Diagnosis. Vietnam. Male with long genitalia, projecting half the length of abdomen in dried specimens; abdomen and genitalia with long, scattered setae; tergum X of males with single setal tuft on each ventro-lateral margin on a raised base at mid-length.

Abbreviations of depository collections
Forewing ground colour and fascial pattern (Figs 1, 2) corresponding widely with the two other known species of Aureopterix Gibbs, 2010. The male genitalia of the new species are more similar to those of A. micans Gibbs, 2010, described from New Caledonia, andless similar to A. sterops (Turner, 1921) distributed in northern Queensland, eastern Australia. A. bachmaensis sp. nov. mainly differs from both species by the shape of the valvae and the slender segment X bearing one single setal brush on a knob-like process of the lateral margin in male genitalia.
Description. (Figs 3-6) Length of forewings 3.9 mm (male) to 4.1 mm (females). Antennae with 34 flagellomeres in male, 32 in female, extending to two-thirds of forewings; first four basal flagellomeres fused, clothed with white lamellar scales, following flagellomeres brown, with long, dark sensillae and ascoids, female flagellomeres 4 to 6 black; head capsule dark brown, with dense tufts of white, piliform scales on frons and vertex; eyes hemispherical; epicranial suture and ocelli absent; clypeus separated from frons by a deep, arched suture extending between the tentorial pits; labrum long, triangular with rounded tip; mandibles present, apical portions hidden under labrum; maxillae with long, five-segmented palpi, held in vertical position close to frons, inner endites two short, rounded processes (= galea and subgalea); labial palpi short, three-segmented, terminal segment with a garland of stiff sensillae. Pronotum and basal part of tegulae brown, dorsum of thorax with silvery white, lamellar scales. Ground colour of forewings pale white, shining silvery, some brown spots at base of costa, apical part of forewings with oblique, bronzy fascia, fringes white, hindwings shining bronzy on upper-and underside. Wing venation ( Fig. 7) with Sc and R1 forked in forewing, simple in hindwing or absent (R1), R4 and R5 in both wings very short, forming forks encompassing the wing tips, hindwings with accessory cell absent, anal veins without looping. Wing coupling mechanism with short jugum of forewings and bundle of three erect bristles on costal base of male hindwings, females without those bristles. Legs with white coxae and femora, tibiae and tarsal segments dark brown, epiphysis present on foretibia, legs clothed with acute tipped scales, long or short spines in addition to spurs absent, spurs 0.0.4. Male abdomen with long bristles on ventral side, glands of sterna V present, orifice rounded, segment VIII of male present as tergum only, no traces of sternite visible.  Flagellomeres, mid-section; 7. Wing venation, holotype; 8. Male abdomen and genitalia, lateral view; 9. Segment X, dorsal view; 10. Male genitalia, ventral view; 11. Female abdomen, lateral view. Scale bars: 0.25 mm (3-5.); 10 µm (6.); 1 mm (7.); 0.5 mm (8.); 0.5 mm (10., 11.); Male genitalia (Figs 8-10): segment IX bulbous, not forming a closed ring, anterior margin of ventral side slightly excavated, valvae very long, club-shaped, tips acute in ventral view; segment X shorter than length of valvae, narrowly cleft at apex for half of its length, paired apices rounded, lateral margin with a brush of 3-4 short setae on a short process directed ventro-mediad; median plate weakly sclerotized, enclosed in basal part of segment X; phallic apparatus long and tubular, terminal part of phallocrypt with micro-spines on dorsal side, distal part of phallus membranous, cornuti absent.
Female genitalia (Fig. 11): segment I to VIII with sclerotized terga and sterna, segment IX elongate, membranous and telescoping, with a continuous sclerotized ring on distal margin, segment X with rounded, lateral sclerites of paired and setose terminal papillae (= papillae anales). (The bursa was completely macerated during boiling in KOH).
Molecular results. (Fig. 2C, Table 1) We recovered only the COI-1a fragment (325bp) for both samples. In the best scoring RAxML-tree the genus Aureopterix is well supported as a monophylum with respect to Zealandopterix and Tasmantrix (BS = 97). Relationships among A. bachmaensis sp. nov., A. micans and A. sterops remain unclear.
Remarks. The locality in the Bach-Ma National Park will probably not remain the only record of this new species. Future field work will provide a more accurate picture of the species range, which is probably restricted to the Truong Son Mountain Range (= Annamite Range). This roughly north to south running mountain range along the Laos-Vietnam border is an area of endemism which gained global recognition in the early to mid-1990s with the discovery of six spectacular mammal species (Sterling and Hurley 2005) that are confined to this range. The report of A. bachmaensis sp. nov. in the National Park is an example from Lepidoptera underpinning the significance of the area.
Etymology. Composed of the generic name Agathiphaga and the added syllable "ma". Diagnosis. Burmese amber, middle-sized species, terminal segments of maxillary palpi annulated, basal segment of labial palpi with dorsal hair-brush, tibial spurs 1.3.4., epiphysis present on short foretibia, forewings with R1 shortly branched into R1a and R1b, female with long, telescoping ovipositor, apophyses posteriores fused in apical half into a single apophysis extending in midline towards slender papillae anales.
The fossil genus differs from extant homoneurous moths of Agathiphaga Dumbleton, 1952 by differences in the morphology of the maxillary and labial palpi, the spur formula 1.3.4.
The flexible form of the terminal segment of the maxillary palpi seems to be due to a mottled loss of sclerotization, which gives the segment an annulated appearance. In Agathiphaga, this segment is very short and not annulated (Dumbleton 1952). Etymology. The specific name is the Latin adjective "perditus", lost, in singular, feminine nominative, referring to the species as an extinct taxon.
Preservation. The holotype is embedded in a large, polished and oval piece of amber (Fig. 32). The adult insect is nearly completely preserved, somewhat distorted and mainly visible in lateral view. The right side from head to thorax is macerated with right fore-and middle legs missing. The right head side is damaged forming a hole into the head capsule. The hindwings are partly covered by the forewings. One small, black Coleoptera species (3 mm length) is present.
Female genitalia (Fig. 17): segment VIII dorso-ventrally flattened, densely covered by short, lamellar scales, segment IX and X forming a long, telescoping oviscapt with unpaired apophysis posterior, visible in the midline of the interior of segments IX and X.
Remarks. This is the first fossil species of the family. It is also the first evidence of the occurrence of the family Agathiphagidae in South-East Asia in the Mesozoic about 100 Ma ago. The morphological differences to Agathiphaga are significant and justify at least the establishment of a separate genus. According to Cruickshank and Ko (2003), the palynological record from the Burmese amber mines in northern Myanmar includes palynomorphs of Araucariaceae. Poinar et al. (2007) confirmed the araucarian source of the amber and suggested a species of the genus Agathis Salisbury as the resin-producing tree (Poinar 2019b). Extant species can secrete large quantities. Mechanical damage such as cutting into the bark of A. dammara (Chambert, 1803) results in large outpourings of resin (Fig. 38). This genus is present in South-East Asia with a number of species occurring in Malaysia and maritime South-East Asia (Michaux 2001). Agathis was considered by Morley (1998) as Gondwanan element which dispersed into South East Asia in the Tertiary. The seeds in the fe- male cones of the trees are the food resource of the two extant species of Agathiphaga, A. vitiensis Dumbleton, 1952 (Fidji, and further West Pacific Islands) and A. queenslandensis Dumbleton, 1952 (Australia, Queensland). The host-plant of Agathiphagama perdita sp. nov. could have been also a species of the gymnosperm family Araucariaceae. Judging from the fairly restricted range of Agathiphaga in the Australian Region (e.g. Dumbleton 1952) the species seems unlikely to have managed to disperse together with its host-plant into South East Asia. Discrepancy in the distribution of host plants and their associated Lepidoptera species is a frequently observed phenomenon. However, the distribution of herbivorous species is not only determined by the occurrence of the host plant but by the combined action of additional biotic and abiotic factors. Missing data, however, can account as well for a seeming absence in an area. The Microlepidoptera fauna of the region is inadequately researched and new records including surprising discoveries seem to be always possible.
The fossil Agathiphagama gen. nov. and the extant Agathiphaga are the only genera of Agathiphagidae. Both genera exhibit the characters of the family, but are probably not closely related due to the differences indicated in the diagnosis. The annulated terminal segments of the maxillary palpi of Agathiphagama gen.nov. seems to be a derived character. It resembles the terminal maxillary palpi of Annulipalpia and some Integripalpia genera (e.g. Athripsodes Billberg, 1820, Ceraclea Stephens, 1829) in Trichoptera. Kristensen (2003: 51) considered the annulated surface of the fourth segment as a lepidopteran ground plan character, but this character is not visible in the fossil specimens.
The Agathiphagidae are the only known family in extant Lepidoptera with four veins in the forewings including remarkable variation in branching pattern (Schachat and Gibbs 2016). This plesiomorphic character is, however, present in the Jurassic families Mesokristenseniidae and Ascololepidopterigidae. The former differs from Agathiphagama and Agathiphagidae in its spur formula 1.1.4 and in the absence of an epiphysis (Huang et al. 2010). The latter differs from Agathiphagidae and Mesokristenseniidae by lacking medial spurs on the metatibiae (Zhang et al. 2013).
Etymology. A noun composed of the Latin "acanthus", thorn and the Latin "corona", crown, alluding to the name Lophocorona and to the long spikes at the bases of the valvae and the spine and denticules on its apical margins, forming a spiny crown when the tips of the valvae are hold close together.
Diagnosis. Burmese amber, small-sized species, antennae short, basal flagellomeres broad, epiphysis present, homoneurous venation, forewings with accessory and median cells present, crossvein r1-r2 present, R5 running to termen (below apex) in both wings; valvae of male genitalia with one or more pairs of long, basal spikes and a terminal, short, rod-like 'thorn'.
This fossil genus differs from extant homoneurous moths of Lophocorona by the presence of an epiphysis (absent in Lophocorona), the presence of crossvein r1-r2 and the joint presence of an accessory and median cell (accessory cell may be present or absent in Lophocorona). The valvae in the male genitalia carry a long, rod-like spine on the ventral tip together with numerous short denticules on the apical margin. In Lophocorona the spine on the ventral tip is small and blunt. The long spikes originating from the inner side of the base of the valvae can be regarded a synapomorphy of Lophocorona and Acanthocorona gen. nov.
Description. Forewing length 3-5 mm, eyes hemispherical, frons and vertex with tufts of long piliform scales, ocelli absent; antennae short, about half the length of forewings, about 25-30 flagellomeres present, flagellomeres scaled on dorsal side, wider than long at base, becoming thinner and slender towards tip of antennae; proboscis present, dissociated into galea halves, maxillary palpi reduced in size, labial palpi upturned, terminal segment swollen, densely clothed by short bristles, tibial spurs 0.2.4., spurs covered by small scales, epiphysis present, legs slender (Fig. 26), with thin and strong spines on lateral and apical sides of tibiae, tips of tarsomeres with pair of short spines, ungues and arolium of praetarsus small; forewing venation (Figs 18, 30) ) with Sc1 and Sc2, simple R1, sectorial veins of R separate, originating from short accessory cell, R5 terminating to termen shortly below tip of forewing; medial cell present, M4 absent; hindwings (Figs18, 30) with Sc and R1 unbranched, accessory and medial cell open, base of costa with a number of short bristles; scales of forewing short and spatulate, or long with apical margins serrated, scales of fringes long, lanceolate, rounded at apex (Fig. 29).
Male genitalia : valvae elongate, band-like, of species-specific shape, with an erect and protruding rod-like, blunt process on ventro-distal corner, directed dorso-mediad, inner side of apical portion or apical margin with short denticules, bases of valvae with one, two or three long spikes, originating from knob-like protuberances or papillae on the inner side; median plate short, of different shape; dorsal median lobe of segment X present or absent, simple or bifid; phallic apparatus, if extruded, a long, slender tube, sometimes dilated on apex, gonopore in apical position.
Female genitalia (Fig. 31): sternum VIII with broad base and triangular ventral apex; segment IX fused with segment IX, oviscapt cone band-like, dorso-ventrally flattened, strongly sclerotized, fuscous to black, apex blunt, oviscapt saw usually hidden in oviscapt cone, sometimes protruding with its acute tip beyond cone margin.
Remarks. Diagnostic characters of Lophocorona Common, 1973 are: 1) absence of an epiphysis, and 2) the long stalk of R4 and R5 in the forewings encompassing the wing apex. These characters are in a plesiomorphic state in Acanthocorona gen nov., with epiphysis present and R4 and R5 in the forewings always running as separate veins from accessory cell to wing margin. However, the structures of the male and female genitalia agree largely with those of Lophocorona. Especially the architecture of the female postabdomen is very similar to those of females of extant Lophocorona species (Nielsen and Kristensen 1996). The nearly complete correspondence of this character complex with Lophocorona Common, 1973 provided the clue for identifying specimens in Burmese amber as lophocoronids. A correct association of males and females in Burmese amber is, however, a difficult venture. There are no unique characters other than genitalia, which would permit combining sexes. The structures of the female postabdomen are described in the generic description, but without assigning female specimens to one of the described males.
Burmese amber contains a surprisingly high number of species attributable to Acanthocorona gen. nov. The individuals are in most cases embedded in an unfavourable position and exhibit only a reduced number of characters. But none of the externally visible traits contradict the diagnosis and description of the genus. Cross-veins are often difficult to see and they may appear to be absent in some individuals. This uncertainty makes the character unreliable and reduces its taxonomic weight. The following species are described and included in Acanthocorona gen. nov. essentially on the basis of the male genitalia. The morphology and arrangements of spines and denticules on apical parts of the valvae constitute the principal character complex, which exhibits a large variety allowing the separation and establishment of different species. The following descriptions of new species are short and concentrate on the male genitalia and their illustrations. The depicted features are diagnostic enough to distinguish the presented species and to identify new species in fresh, additional material of Burmese amber, which hopefully will continue to become available for scientific study in the future. Etymology. The species is named in memory of Andrzej Skalski, who published the first record of a lophocoronid specimen from Asia (Skalski 1979), an interpretation later considered very tentative by Kristensen and Skalski (1998).
Preservation. Completely preserved in a nearly rectangular piece of amber, wings somewhat spread, but overlapping, head, legs and postabdomen clearly visible (Fig. 34).
Male genitalia (Figs 19,20): segment IX with short, median prolongation in dorsal view, presumed median plate below this prolongation bilobed; rod-like spine on ventral apex of valvae long and straight, apical margin of valvae with denticules, and some additional denticules before margins; basal spikes of valvae paired, longer as length of valvae, sitting on elongate papillae from median side of valvae, a third median pair of bristles present, shorter than basal spikes. Phallus not visible. Etymology. The species is named in honour of Patrick Müller, collector of amber inclusions, for providing material for scientific study.

Acanthocorona muelleri
Preservation. Completely preserved in a flat, oval piece of amber (Fig. 35), wings overlapping, legs and post-abdomen well visible in ventral view, air bubble on mouthparts and prosternum, additional insects present (two Hymenoptera, two Diptera, one Collembola).
Description. Length of forewings 3.0 mm, antennae brown, 23 flagellomeres. Male genitalia (Figs 21,36): rod-like spine on ventral apex of valvae long, straight and thickened, apical margin of valvae with three denticules of declining size, no denticles before margins; basal spikes of valvae paired, slightly shorter than length of valvae, arising on elongate papillae at median sides of valvae. Phallus long, tubular and gradually curved ventrad, tip with short, protruding vesica.
Preservation. Completely preserved on the margin in a large, drop-like piece of amber, wings somewhat overlapping, distorted, legs and post-abdomen clearly visible.
Description. Length of forewings 3.6 mm, antennae dark brown, 24 flagellomeres. Male genitalia (Fig. 22): length of valvae as long as half the length of abdomen; rod-like spine on ventral apex of valvae long and straight, apical margin of valvae with row of denticules, no denticles before margins; basal spikes of valvae paired, slightly shorter than length of valvae, sitting on elongate papillae from median side of valvae. Phallus extremely long, slightly curved ventrad, ventral side of apex with elongate slit revealing short teeth. Etymology. The species is named in honour of Wilfried Wichard for providing material and taking photos of Microlepidoptera of Burmese amber.
Preservation. Completely preserved in an oval piece of amber with much particulate detritus particles and some air bubbles, wings overlapping, legs and post-abdomen clearly visible in ventral view, one additional insect specimen present (one female of Hydroptilidae, Trichoptera, a single minute Coleoptera).
Male genitalia (Fig. 23): segment IX with median prolongation; rod-like spine on ventral apex of valvae absent, replaced by a bulbous area with short and long bristles, apical part of valvae enlarged forming an oval lobe with short denticules of on inner side, no denticles on margins, inner side of valvae with long spine, directed dorso-mediad; basal spikes of valvae absent; median plate short, rectangular in ventral view. Phallus long, tubular and curved ventrad.
Remarks. A. wichardi sp. nov. differs from the remaining species of the genus by lacking spines on the legs, absence of basal spikes and apical, rod-like spines of the valvae. The presence of a long spine on the median side of the valvae instead of emerging on the ventral corner is a unique character. The species is provisionally included in the genus until better preserved material becomes available which may lead to a different systematic placement.
Preservation. Completely preserved in a round, polished piece of amber, but not clearly visible due to several fractures in the amber; numerous small bubbles of air present; wings overlapping, legs and postabdomen clearly visible.
Male genitalia (Fig. 24): segment IX with short,triangular, median prolongation in ventro-caudal view; rod-like spine on ventral apex of valvae short, apical margin of valvae with row of five denticules, no denticules on inner side before margins; one pair of basal spikes of valvae present, about 1/3 the length of valvae. Phallus not visible.

Acanthocorona sattleri sp. nov.
http://zoobank.org/5638DDFF-C5C3-4592-B8CC-A5EEF7F1B935 Etymology. The species is named in honour of Klaus Sattler, London, specialist of Microlepidoptera in the Natural History Museum, London, for his support and help during many visits of the first author to the Microlepidoptera collection in London.    Preservation. Completely preserved in a flat, rounded and polished piece of amber, numerous small bubbles of air and two, minute midges (Diptera) present; wings overlapping, head, legs and postabdomen clearly visible in ventral view.
Description. Length of forewings 2.9 mm, antennae light brown, very short, about 0.3 of forewing length, with 21 flagellomeres.
Male genitalia (Fig. 25): segment IX rounded dorsally, segment X with short, bifid median prolongation in latero-dorsal view (Fig. 25A); rod-like spine long, accompanied by shorter spines on ventral apex of valvae, apical margin of valvae with row of denticules, additional denticules before margins; basal spikes of valvae paired, about half the length of valvae (Fig. 25B). Phallus not extruded.
Etymology. The specific epithet is composed from Latin "spina", spine, and "fero", to carry, referring to the strong spines on tibiae of the adult moth.
Preservation. Completely preserved in a small, rounded, polished piece of amber, embedded in dorso-ventral position, with right wings spread out, some short fractures and few a bubbles of air present, legs and postabdomen well visible (Fig. 37).
Description. Length of forewings 4.8 mm, antennae dark brown, less than 0.5 of forewing length, with 30 flagellomeres; scales of forewing short and spatulate, or long with apical margin serrated, scales of fringes long, lanceolate, rounded at apex (Fig. 29).
Male genitalia (Figs 27,28): segment X a large dorsal plate with deep, triangular excision of apical margin giving the structure a bifid form (Fig. 28); valvae broad, somewhat enlarged and rounded on apices; rod-like spine on ventral apex of valvae long, apically truncate, not accompanied by shorter spines, apical margin of valvae without denticules, basal spikes of valvae paired, about 0.8 the length of valvae (Fig. 27). Phallus not extruded.
Female genitalia (Fig. 31): sternum VIII with broad base and triangular ventral apex; segment IX fused with segment IX, oviscapt cone band-like, dorso-ventrally flattened, strongly sclerotized,   A B fuscous to black, apex blunt, oviscapt saw usually hidden in oviscapt cone, sometimes protruding with its acute tip beyond cone margin.
Remarks. These female specimens cannot be assigned to any of the named species at the moment (see under remarks in the genus description). Since the female genitalia is an important character complex for the recognition of the family, the genitalia of one individual (NIGP 173719) was illustrated. The genitalia of the second species are difficult to see but are identifiable as those of a female.

Discussion
This paper aims to complete the picture of the distribution and diversity of past and recent primitive moths. A formal biogeographic analysis or providing a comprehensive review of recent and past distributions was beyond the scope of this study. The following discussion aims to guide any future biogeographical studies on primitive moths of South-East Asia, as well as to foster further works on Lepidoptera fossils. Wagner and Davis (2014) discovered Neotropical taxa of Micropterigidae occurring in Costa Rica and reported the first example of a genus range in the family stretching over both sides of the Equator (Squamicornia). Aureopterix is now another example of a micropterigid genus with records from the Northern and Southern Hemisphere, but in this case, oceans divide the disjunct parts of the generic range. The distance between the disjunct ranges of A. bachmaensis and the other two known species is about 6000 km on a northwest-southeast axis. Knowledge of the microlepidopteran fauna of the Larger and Smaller Sunda Islands as well as of New Guinea is poor, and thus we cannot exclude the possible occurence of Micropterigidae in these regions. The notion of a continuous distribution of Aureopterix in the Indo-Australian Archipelago, today or in the past was our initial hypothesis, considering the many documented examples of this distribution type in Lepidoptera (Holloway 1998;Holloway and Nielsen 1998;Holloway et al. 2001;De Jong 2001).

Aureopterix bachmaensis sp. nov.
Dispersal and colonization processes are closely related to the tectonic structure and geological and climate history in South East Asia, Melanesia and the Southwest Pacific. Kitching et al. (2001) and De Jong (2001) analysed the distribution pattern of butterflies and suggested a number of hypotheses which are synthetical explanations including tectonic, evolutionary and ecological processes with dispersal as important mechanism. In contrast to butterflies, thought to have originated around 119 Ma ago (Espeland et al. 2018) primitive homoneurous families of Lepidoptera are much older and have already existed during periods of tectonic movements 180 Ma ago in the Early Jurassic (Ansorge 2002;Grimaldi and Engel 2005). The basal splitting event among known extant Lepidoptera is presumed to have given rise to the Micropterigidae (Kristensen and Skalski 1998;Wahlberg et al. 2013;Regier et al. 2015;Kawahara et al. 2019) and its sister group, the bulk of the Lepidoptera. The family has a widely scattered cosmopolitan distribution, which might suggest a Pangaean origin. In a continental drift scenario and/or any relevant independent dating, disjunct distribution patterns in this family can also be explained by providing vicariance-driven scenarios based on tectonic history reaching back into the Mesozoic. Recently, for example, Mielke (2018, 2020) proposed such a vicariance model for explaining the distribution of the homoneurous Hepialoidea in the Southwest Pacific area.
In a molecular study of the radiation of the micropterigid genus Sabatinca Walker, 1863 in New Caledonia and New Zealand using COI-5P, both species of Aureopterix known for the Australian region were included (Gibbs and Lees 2014). According to the dating analysis of these authors based also on fossil calibrations, the Australia-New Caledonia split in Aureopterix is ca. 54 Ma old (95% interval: 40-74 Ma) and the branching of Aureopterix and Zealandopterix in their chronogram was estimated at ca. 83 Ma (95% confidence interval: 62-102 Ma). These dates substantially postdate the timing of the breakup of East Gondwana into Madagascar+India and into Australia, New Zealand and Antarctica at ca. 130 Ma based on palaeomagnetic dates (McIntyre et al. 2017), after the presumed detachment of terranes from northern Gondwana predicted from its geology at ca. 120 Ma (Metcalfe 2001(Metcalfe , 2017. Thus, the vicariance scenarios are not in agreement with the age and phylogeny-based divergence times of Aureopterix and related taxa as documented in Gibbs and Lees (2014), who also noted such a conflict in the split of A. micans and A. sterops. If this phylogenetic dating is accurate, we have to consider alternative, dispersal processes as the main driver in shaping the disjunct range of Aureopterix, rather than passive transport on continental terranes or vicariance via submerged parts of ancient continents. The recovering of Aureopterix within a clade including the stricly Australasian genera Tasmantrix and Zealandopterix suggests an Australasian origin of Aureopterix, with a long-distance dispersal for A. bachmaensis being the most probable scenario. The discovery of this genus in Vietnam is remarkable since the overseas dispersal scenario is rather hard to imagine because these taxa are moist forest dwellers, essentially confined to the substratum with larvae and adults highly prone to desiccation when leaving their habitats (Lorenz 1961). The biology of Aureopterix is not known yet, but host plant were shown to be strictly conserved in Micropterigidae of Japan, all feeding on the liverwort Conocephalum conicum. Gibbs and Lees (2014) also acknowledged a weak dispersal power in Micropterigidae. There might be other dispersal mechanisms we are unaware of, or the geological history of continental terranes, including the context with neighbouring oceanic islands or island arcs seem to be imperfectly known to date (for example geological uncertainties about submerged continents such as in the Australian region Zealandia), or both.

Agathiphagidae, Lophocoronidae
The stunning discovery of extinct taxa of primitive Lepidoptera in Myanmar, which were thought to be restricted in their distribution to the Australian Region, substantially revises present notions on the historical biogeography of Lepidoptera groups. In the absence of fossil distributions, Agathiphagidae and Lophocoronidae seem like classic cases of endemism in the Australian Region. Agathiphaga has two known species and stretches across the Pacific to Solomons, Vanuatu and Fiji and is thought to have benefitted from the possibility of long diapause in drifting Agathis seeds (Upton 1994). The biology of Lophocorona, by contrast, is still unknown. The fossil species of Agathiphagidae and Lophocoronidae found in Myanmar might alternatively provide evidence of a wider ancestral distribution of the two families, if such oceanic dispersal mechanisms do not prove to be a significant transport mechanism. The hypothesis that their extant ranges in the southern Hemisphere are relicts of a previous intercontinental distribution encompassing Asia and Australia has not yet been tested.
The time of divergence for lineages leading to the families Agathiphagidae and Eriocraniidae+Lophocoronidae was estimated by Wahlberg et al. (2013) at around 160 Ma (Agathiphagidae) and at around 180 Ma (Eriocraniidae+Lophocoronidae). At this time, in the Early to Late Jurassic, the distribution and positions of continents were quite different from their configuration today. The increasing separation of Laurasia and Gondwana by the Tethys ocean occurred in the Jurassic and was completed in the Cretaceous (Metcalfe 2017). This long period in earth history allows for proposing hypotheses which explain present distribution patterns in terms of passive transport on continental plates.
From a historical perspective, the Oriental fauna is a mixture of tropical Laurasian and Gondwanan taxa, over which is overlaid the results of dispersal processes. The collision of the Indian subcontinent into Asia in the early Eocene brought elements of the Gondwana fauna to the north and resulted in a pronounced enrichment of the biota (Morley 1998). Long before the accretion of India, several terranes were detached from the margin of North-East Gondwana and were shifted to the north during the Jurassic. They arrived at Laurasia and became part of the Asian continent during the Cretaceous (Metcalfe 2017). With the movement of these continental terranes, ancient biota could have been transported, and given permanent over-water conditions of the terranes during the passage, arrived in Asia and immigrated into the resident biota. Based on this geological scenario, the extant occurrence and distribution of the Gondwanan caddisfly family Hydrobiosidae (Trichoptera) in Asia were explained by a vicariance/dispersal model (Mey 1998). Further examples of this terrane transport from angiosperms and invertebrate groups with disjunct ranges in Asia and Australia were provided by Poinar (2019b), underpinning the explanatory value of this model of shifting terranes. The occurrences of Agathiphagidae and Lophocoronidae during the Mesozoic in Asia can be explained likewise as a result of a transport by northward drifting Gondwana terranes. So far there have been practically no molecular or other analyses that might seriously test such models.