100 million years of morphological conservation in bark beetles (Coleoptera: Curculionidae: Scolytinae)

Abstract Scolytine weevils (bark and ambrosia beetles) have a unique ecological significance in forest ecosystems, which equates to major effects on landscape ecology and to monetary losses. Fossilized galleries of scolytines have been reported in Late Mesozoic wood, but here we describe a well‐preserved body fossil from the Cretaceous, c. 100 Ma, preserved in amber from northern Myanmar. Moreover, the specimen is remarkably similar to Recent species of the genus Microborus, revealing stasis unexpected within scolytines and thus highlighting the antiquity of the group. Stratigraphic dating and comparison of insect palaeofaunas included in other well‐dated ambers from multiple sites support the age estimate of the Burmese amber. A minimum age for one clade of scolytines is thus established, indicating an early divergence of scolytines from other weevils in the Late Jurassic or Early Cretaceous and challenging the current perspective of weevil evolution.     

Termite coprolites (Insecta: Isoptera) from the Cretaceous of western France: A palaeoecological insight

This paper presents fossil faecal pellets - also named coprolites or frass - attributed to termites, which were found in amber and lignitic clay from the Wealden (Hauterivian-Barremian?), Late Albian and Early Cenomanian of south-western France. These coprolites have a characteristic subcylindrical shape and hexagonal transverse section and are assignable to Microcarpolithes hexagonalis Vangerow. The termite families that possibly produced these coprolites are discussed. The noticeable lack of termite attacks on the fossil wood associated with amber and lignitic clay is taphonomically analyzed in relation with the palaeoflora and palaeoclimate of these amber forests. The different medium where coprolites were found (amber, wood, sediments) suggests that primitive Cretaceous termites had already developed various biologies, such as wood or cryptic foraging, but probably not yet soil-feeding.     

Thrips (Thysanoptera, Insecta) from the Rovno amber, Eocene of Ukraine

Seventy-six thrips were discovered in Rovno amber. Among these, 67 were identified to suborder, 52, to family, 45, to genus, and 41, to species level. In total, five species, six genera, five families, and two suborders are recorded. No undescribed taxa have been found so far. All the identified thrips, except those of the genus Phloeothrips, belong to fossil taxa, previously known only from the Baltic and Bitterfeld ambers. However, the composition of species in the Rovno amber is highly unusual due to domination of Praedendrothrips avus Priesner, 1924. This species, rare in the Baltic amber, constitutes 49% of all the Rovno records. Thus, the Rovno amber, in contrast to the Baltic and Bitterfeld ambers, is characterized by poor taxonomic diversity of thrips and presence of a clearly dominant species.     

Protist-like inclusions in amber, as evidenced by Charentes amber

The mid-Cretaceous amber of France contains thousands of protist-like inclusions similar in shape to some ciliates, flagellates and amoebae. The sheer abundance of these inclusions and their size variation within a single amber piece are not concordant with true fossil protists. French amber is coniferous in origin, which generally does not preserve well protists without cell walls. Thus, it would be surprising if French Cretaceous amber had preserved millions of protists. Here, we present a survey of the protist-like inclusions from French amber and attempt to elucidate their origins.Diverse Cretaceous ambers (from Spain, Germany and Lebanon), also derived from conifer resins, contain thousands of protist-like inclusions. In contrast, Tertiary ambers and modern resins are poor in protist-like fossils. This suggests these inclusions originated from early Cretaceous plant resins, probably secreted with the resin by trees that did not survive after the Cretaceous (such as the Cheirolepidiaceae). A review of the recent literature on amber microfossils indicates several protist-like inclusions that are unlikely to have a biological origin have already been described as real fossil protists. This is problematic in that it will bias our understanding of protist evolution.     

Eohelea sinuosa (Meunier, 1904) (Diptera, Ceratopogonidae) in Late Eocene ambers of Europe

Differences between ceratopogonid faunas from different Late Eocene ambers are almost as great as between ant faunas and give evidence of their different geographical origins. The greatest similarity is recorded between ceratopogonid faunas of the Rovno and Danish ambers; it manifests itself, in particular, in the presence of Leptoconops, abundant Eohelea sinuosa, and rather frequent occurrence of Meunierohelea. Eohelea sinuosa is the most abundant ceratopogonid species in the Rovno amber. The abundance of Eohelea is probably accounted for by the abundance in these assemblages of small chironomids, with terrestrial larvae; which composed 40% of the Rovno amber chironomid fauna and were probably prey to Eohelea. It is shown for the first time that Ceratopogonini with feminized male antennae (with reduced plume) occur three times as often in syninclusions of specimens of both sexes (63% of all Eohelea inclusions from the Rovno amber);this is evidence that Ceratopogonini with feminized male antennae turned to mating on substrate. This supports the hypothesis of Dinwiddie and Rachootin (2011) that wing organs of female Eohelea were not used for stridulation.     

Miocene spiders in Dominican amber (Oonopidae,Mysmenidae)

Oonops seldeni sp. nov. and Mysmenopsis lissycoleyae sp. nov. are described from male specimens preserved in Miocene amber from the Dominican Republic and are the first fossil records of these extant genera. Gamasomorpha incerta Wunderlich, 1988 is transferred to Stenoonops. Two females previously described as Orchestina dominicana? Wunderlich, 1981 are transferred to Orchestina sp. indet., and one new specimen of a male of Orchestina dominicana Wunderlich, 1988 is identified. Oonopidae is reported for the first time from Cretaceous ambers of Burma, Lebanon and New Jersey. These are the oldest records of this family, extending the known range from the Rupelian (Oligocene) to the Valanginian (Lower Cretaceous). Recent StenoonopsMysmenopsis are unknown from Hispaniola. The presence of these genera in amber suggests that they will be found. The presence of Mysmenopsis in amber is further evidence of kleptoparasitic/commensal spiders in the Miocene.     

Microbe‐like inclusions in tree resins and implications for the fossil record of protists in amber

During the past two decades, a plethora of fossil micro‐organisms have been described from various Triassic to Miocene ambers. However, in addition to entrapped microbes, ambers commonly contain microscopic inclusions that sometimes resemble amoebae, ciliates, microfungi, and unicellular algae in size and shape, but do not provide further diagnostic features thereof. For a better assessment of the actual fossil record of unicellular eukaryotes in amber, we studied equivalent inclusions in modern resin of the Araucariaceae; this conifer family comprises important amber‐producers in Earth history. Using time‐of‐flight secondary ion mass spectrometry (ToF‐SIMS), we investigated the chemical nature of the inclusion matter and the resin matrix. Whereas the matrix, as expected, showed a more hydrocarbon/aromatic‐dominated composition, the inclusions contain abundant salt ions and polar organics. However, the absence of signals characteristic for cellular biomass, namely distinctive proteinaceous amino acids and lipid moieties, indicates that the inclusions do not contain microbial cellular matter but salts and hydrophilic organic substances that probably derived from the plant itself. Rather than representing protists or their remains, these microbe‐like inclusions, for which we propose the term ‘pseudoinclusions’, consist of compounds that are immiscible with the terpenoid resin matrix and were probably secreted in small amounts together with the actual resin by the plant tissue. Consequently, reports of protists from amber that are only based on the similarity of the overall shape and size to extant taxa, but do not provide relevant features at light‐microscopical and ultrastructural level, cannot be accepted as unambiguous fossil evidence for these particular groups.     

Review of the Late Eocene Encyrtidae (Hymenoptera,Chalcidoidea) with a description of the first fossil genus with filum spinosum

Glaesus gibsoni gen. et sp. nov. and Eocencnemus gedanicus sp. nov. are described from materials stored in the amber collection of the University of Gdańsk. Eocencyrtus zerovae Simutnik, 2001 is for the first time recorded in the Baltic amber. The encyrtids recorded in Eocene ambers are reviewed, and a key to the known genera is given. The fossil Encyrtidae cannot be placed with confidence in any of the established subfamilies. Their comparative morphology is analyzed. One of the diagnostic characters of the subfamily Encyrtinae, the presence of the filum spinosum, is recorded for the first time for fossil encyrtids (in G. gibsoni).     

Leonophyllum tenellum nov. gen., nov. sp., an enigmatic plant from the Early Jurassic of the Mecsek Mts (Hungary)

The Early Jurassic flora of the Mecsek Mountains is diverse, with numerous representatives of ferns, seed ferns, cycadophytes, ginkgophytes, and conifers. Its (para-)autochthonous deposition, good preservation and low collection bias has permitted researchers to save delicate, small plant remains that would generally be missing from the fossil record. These plant fossils are characterized by having a “filmy” (probably unilayered) structure, thin stalks with flat leaf-like branches and ultimate irregular segments with streamlined epidermal cells having thick cell walls. Due to the absence of sporangia, the plant remains cannot be confidently assigned to any higher plant group, although they show some similarities to thalloid liverworts with raised vegetative bodies and also have some resemblance to the fern family Hymenophyllaceae. The new genus and species Leonophyllum tenellum Barbacka et Kustatscher is erected.     

Charles de Gerville et les premiers restes de Plesiosauria signalés dans le Jurassique inférieur de France (Hettangien,région de Valognes,Manche)

The historian, archaeologist, and naturalist Charles de Gerville (1769–1853) reported as early as January 1816 the presence of fossil bones in the quarries of the region of Valognes, in the department of Manche. These quarries exploited the “Calcaire de Valognes” and the underlying “Argiles et Calcaires d’Huberville”, both formations dated as Lower Hettangian (Lower Jurassic). De Gerville communicated to Jacques-Louis-Marin Defrance a watercolour drawing of one of these fossil bones, discovered in July 1820, in which it is possible to recognize a plesiosaur femur. This femur, as well as a fragment of rib and three vertebrae of Plesiosauria from de Gerville's collection, was then figured in a publication by Arcisse de Caumont, in 1825. The plesiosaur femur was later acquired by Pierre Tesson of Caen, who owned one of the most important collections of fossils in Normandy. The Tesson collection was later purchased in 1857 by the British Museum (now The Natural History Museum, London), where the femur has been rediscovered. This specimen is the first known plesiosaur specimen ever discovered in the Lower Jurassic of France, before the genus Plesiosaurus was established upon material from the Lias of southwestern England. One of the vertebrae figured by de Caumont has been rediscovered in the “Muséum Emmanuel-Liais” (Cherbourg-en-Cotentin), which had acquired part of de Gerville's collection. The interpretation of the “fossil bones of Valognes” by Georges Cuvier, Henri Marie Ducrotay de Blainville, Arcisse de Caumont, Jacques-Amand Eudes-Deslongchamps and Constant Duméril is revealed through unpublished documents.     

First fossil horsefly (Diptera: Tabanidae) in Miocene Mexican amber

The fossil record of the Tabanidae is sparse when compared with other families of Diptera. Even in amber they are rare, probably because of their size and specific flight behavior. Horseflies from amber are only known from Cretaceous age New Jersey amber as well as from the Tertiary age Baltic and Dominican amber, but are herein described for the first time, with Stenotabanus oleariorum sp. n., from Mexican amber. The new species is compared to the fossil horseflies of the same genus S. brodzinskyi Lane, Poinar and Fairchild 1988 and S. woodruffi Lane and Fairchild 1989 from Dominican amber.     

L’ambre albo-cénomanien de la montagne de Lure (Alpes-de-Haute-Provence), outil stratigraphique et paléogéographique

Nodules of fossil resin or amber, first drifted and then deposited in the marine series with cephalopods, were discovered in several areas of High-Provence, in geological series of the Cretaceous system. These areas are located around the Mountain of Lure; amber nodules have been found in the upper Albian (Ongles, Revest-des-Brousses) and in the lower Cenomanian (Saint-Étienne-les-Orgues, Aubignosc and Salignac). These ambers have very homogeneous and characteristic FTIR spectra, making it possible to distinguish them not only from more recent ambers of the upper Cretaceous of Provence (Santonian), but also from tertiary ambers of the Baltic sea. These organic matters in marine environment, brought by the currents and deposited in shallow waters of the Ventoux-Lure area, are in agreement with close emerged grounds, which were set up by the Albo-Cenomanian tectonic movements.     

A new genus and species of fossil scorpion (?Euscorpiidae) from the Early–Middle Eocene of Pesciara (Bolca,Italy)

Fossil scorpions are among the oldest terrestrial arthropods known from the fossil record. They have a worldwide distribution and a rich fossil record, especially for the Paleozoic. Fossil scorpions from Mesozoic and Cenozoic deposits are usually rare (except in amber-deposits). Here, we describe the only fossil scorpion from the Early to Middle Eocene Pesciara Lagerstätte in Italy. Eoeuscorpius ceratoi gen. et sp. nov. is probably a genus and species within the family Euscorpiidae. This may be the first fossil record of the Euscorpiidae, which are so far only known from four extant genera. Eoeuscorpius ceratoi gen. et sp. nov. was found in the “Lower Part” of the Pesciara Limestone, which is actually dated Late Ypresian stage (between 49.5 and 49.7 Ma). Besides a possible pseudoscorpion, the here-described fossil scorpion is the second arachnid species known from the Bolca Locality.     

New species ofElectribius Crowson 1973 (Coleoptera: Artematopodidae) from Baltic amber

Three new species of the genusElectribius Crowson 1973 (Coleoptera: Artematopodidae),E. friederichi, E. balticus, andE. procerus are described from the Baltic amber. The characters separating the extant and fossil species ofElectribius are summarised in a key. A list of the known extant and fossil species of Artematopodidae sensuLawrence (1995) with synonyms and remarks on the geographical distribution is provided. The distribution of the members of the family and the identical morphological specializations of the fossil and extant species ofElectribius suggest that the taxon formerly had a much wider distribution and is relatively old. The possibility that the Upper Jurassic to Lower Cretaceous generaSinoelaterium Ping 1928and Artematopodites Ponomarenko 1990 represent early members of the Artematopodidae is discussed.     

Miocene Ethiopian amber: A new source of fossil cryptogams

Amber is renowned for the exceptional preservation state of its inclusions, allowing detailed morphological analysis and providing relevant environmental, palaeoecological, geographical, and geological information. Amber deposits are predominantly known from North America, Europe, and Asia, and are considered to be rare on the continents that formed Gondwana. The recent discovery of fossiliferous amber deposits in Ethiopia, therefore, provides an inimitable opportunity to close gaps in the fossil record of African terrestrial biota and to study organisms which are otherwise rare in the fossil record. Here we show that diverse cryptogams are preserved in highest fidelity in Miocene Ethiopian amber. We describe gametophyte fragments of four liverworts: Thysananthus aethiopicus sp. nov. (Porellales, Lejeuneaceae), Lejeunea abyssinicoides sp. nov. (Porellales, Lejeuneaceae), Frullania shewanensis sp. nov. (Porellales, Frullaniaceae), and Frullania palaeoafricana sp. nov. (Porellales, Frullaniaceae). Furthermore, we describe a pleurocarpous moss of the extant genus Isopterygium (Hypnales, Pylaisiadelphaceae) and a lichen representing the order Lecanorales. These new specimens represent the first amber fossils of liverworts, mosses, and lichens from the African continent and render Ethiopian amber as one of the few worldwide amber deposits preserving bryophytes (mosses and liverworts) or lichens. Fossil species of Thysananthus were recorded in Eocene Baltic and Oligocene Bitterfeld as well as Miocene Dominican and probably also Miocene Mexican ambers. Fossils that can unequivocally be assigned to Lejeunea have only been found in Dominican amber so far. Neotropical ambers contain only one taxon of Frullania to date, while the genus is most diverse in Baltic, Bitterfeld, and Rovno ambers, formed in temperate regions. The new fossils support a tropical to subtropical origin of Ethiopian amber. The new African liverwort fossils are included in an updated list of leafy liverworts described from worldwide Cenozoic ambers to date.     

缅甸琥珀内含物形态结构在X射线下的可辨识性

【目的】产自缅甸北部胡康河谷的缅甸琥珀形成于白垩纪中期。其艺术价值很高,同时其内含物的生物多样性程度也很高,故其科学价值也不可估量。显微CT能够提供化石(琥珀)内部解剖结构的高分辨率断层图像,故该方法日渐成为目前琥珀研究中的常用方法之一。然而在可见光下可见的琥珀内的生物结构,在X射线下却有不同的结果,这与现生研究材料在显微CT下的表现非常不同。本研究对产自胡康河谷的9块缅甸琥珀进行显微CT检测,试图对这个特殊的现象进行较为系统的解读。【方法】利用数码相机(Nikon 5200D)拍摄琥珀照片,并用Helicon Focus 5.3软件合成。通过显微CT技术扫描琥珀和计算机断层重建技术重建出缅甸琥珀内含物的三维结构形态。【结果】显微CT检测结果主要分为3种:完全无衬度、部分结构有衬度和整体结构有较好衬度。本研究对有较好衬度的琥珀内含物进行了三维重建,展示了琥珀内含物的外部和内部三维结构。【结论】琥珀内含物的可见光成像和X射线成像不存在一一对应关系,其原因和琥珀保存的好坏以及琥珀的密度差、琥珀围岩之间的对比度差异有关。琥珀形成和埋藏过程中的物理和化学变化非常复杂,其机理的探究也更为复杂和困难,本文对这个现象的主要类型做了较为初步的阐述,后续研究需要更为全面的选样和更为严格的实验设计才能够最终解决这个埋藏学上的难题。     

The Range of Bioinclusions and Pseudoinclusions Preserved in a New Turonian (~90 Ma) Amber Occurrence from Southern Australia

A new Turonian amber occurrence, representing the oldest in situ amber locality in Australia and the southern-most locality in Gondwana, has recently been discovered in the Otway Basin of Victoria. The amber was collected from petroleum cores and many pieces contain a range of inclusions that can provide information on the depositional history of the resin. To date, one species of fern spore (Cyathidites minor) and one species of lycophyte spore (Kraeuselisporites sp?) have been conclusively identified in the amber, along with filamentous microorganisms and degraded plant matter. Several samples are also rife with pseudoinclusions as reported recently in other ambers. The abundance of preserved particulate debris and wind dispersed spores suggest that the Otway amber formed subaerially. Furthermore, based on the range of bioinclusions and forms of pseudoinclusions preserved within a single piece of amber, the locus of hardening for individual samples is variably interpreted as occurring in the tree tops, on the tree trunk or on the ground surface. Notably, specific inclusion assemblages are associated with certain colours of amber. By extension, and in accordance with recent studies, amber colour may be indicative of depositional environment. Variation in the environment of solidification may, therefore, be sufficient to account for the broad range of morphological characteristics preserved in a single amber deposit.     

Four new Laniatorean harvestmen (Arachnida: Opiliones) from mid-Cretaceous Burmese amber

Four new laniatorean harvestmen specimens (Arachnida: Opiliones: Laniatores) are described from the mid-Cretaceous (upper Albian–lower Cenomanian) Burmese amber of Northern Myanmar. One is placed as Insidiatores indet., but is not formally named as it is probably immature. Burmalomanius circularis n. gen. n. sp. and Petroburma tarsomeria n. gen. n. sp. represent the first fossil records of the extant families Podoctidae and Petrobunidae respectively. Finally, Mesodibunus tourinhoae n. gen. n. sp. belongs to Epedanidae, a family previously recorded from Burmese amber. These new records bring the total number of Burmese amber laniatorean species to ten, and the total number of fossil laniatoreans to fifteen. The new finds offer additional calibration points for the Laniatores tree of life and are consistent with the hypothesis that the modern Laniatores fauna of Southeast Asia may have had Gondwanan, as opposed to a Laurasian, origins.