Showing posts with label Beetles. Show all posts
Showing posts with label Beetles. Show all posts

Saturday, 24 August 2024

Using microfossils and pollen to determine the origin of a set of stocks in the collection of the Rijksmuseum, Amsterdam.

In 2019 a man donated a set of stocks to the Rijksmuseum in Amsterdam, which he claimed his  grandfather had acquired in the  1970s from a farm in Zeeland Province.  The museum put the stocks on display in 2021, as part of an exhibition about the Dutch colony in Brazil between 1630 and 1654. In 2023, the stocks were loaned to the United Nations in New York, where they formed part of an exhibition about slavery in Dutch colonies. However, during the New York exhibition, questions were raised as to whether the stocks had ever actually been to South America. A radiocarbon analysis suggested that the tree from which the stocks had been made was probably felled in about 1800, with the stocks probably being made in the first quarter of the nineteenth century. Furthermore, DNA testing established that the wood came from a lineage of Oak trees, which today is found growing in Europe between northern Spain in in the south and southern Scandinavia in the north. 

In a paper published in the journal Review of Palaeobotany and Palynology on 10 August 2024, Hans Piena of the Vrije Universiteit Amsterdam, the Dutch Open Air Museum, and the Royal Netherlands Historical Society, Bas van Geel of the University of Amsterdam, Tom Hakbijl of the Naturalis Biodiversity Center, Arie Kalis of Goethe University, Pim van der Knaap and Jacqueline van Leeuwen, also of the University of Amsterdam, and Kees Nooren of Utrecht University, describe the results of a study which looked at palynological evidence (preserved pollen and spores) to develop a forensic picture of the environment in which the stocks had been used.

Oak stocks in the collection of the Rijksmuseum in Amsterdam (Inv.nr. NG.2019–502). Measurements: 265 × 37.5 × 23 cm. Piena et al. (2024).

Sediment was extracted from holes and cracks in the stocks, and analysed for palynomorphs (pollen, algae and spores), and the surface of the stocks were analysed for surface wear and other traces of use.

The stocks comprise two oak beams resting on a pair of cross-braces. Each beam has nine semicircular openings, which correspond to similar openings on the other beam, with the pair making a hole. on the other beam. At one end of the beams is an iron hinge, at the other an obliquely worn padlock eye. The insides of the holes have been smoothed to a shiny surface, suggesting that the stocks were used frequently. The upper surface of the beams are also smooth, having apparently been rubbed frequently with sand; cracks and small holes on this surface were filled with sediment. There are also a large number of chopping and cutting marks on the upper surface, in places forming a chequerboard pattern. The underside shows no signs of similar wear or sanding, and is largely free of sediment. 

The two cross-braces yielded traces of attacks by Fungi and Woodworm, which are not seen on the beams, and are interpreted by Piena et al. as feet upon which the stocks sat. They were previously interpreted as side braces in the two slavery exhibitions, which would have led to the stocks being horizontal, holding prisoners seated on the floor. Under Piena et al.'s interpretation, the holes would have been vertical, forcing anyone  trapped in the stocks to stand.

The number '22' has been written on the upper surface of the stocks in blue chalk. The fact that this has not been rubbed of strongly suggests that it was written after the stocks ceased being used, possibly as part of an inventory process or auction sale. Before the twentieth century, chalk could be produced in few colours other than white, but blue is one of those colours, making it possible the number was written in the nineteenth century. 

The contents of a sediment-filled hole on the upper surface of the stocks were analysed for siliceous microfossils. This produced about 500 000 Diatoms per gram of sediment, with fifty different species identified. These were largely indicative of a mesotrophic freshwater environment, such as a slow-flowing stream or ditch.  This included the epiphytic Diatom Cocconeis placentula, which grows on the surface of aquatic Plants or Macroalgae. No marine or brackish water species were found. Phytoliths (opaline silica crystals which build up in the leaves of Plants as dissolved monosillicic acid taken up with groundwater and precipitated out as water is lost from the leaves via transpiration) associated with Grasses were found, but none associated with Palms. Also present in great numbers were the stomatocysts of Chrysophytes (Golden-brown Algae), which are also typical of freshwater environments, with about 460 000 stomatocysts per gram of sediment. Also present were samples of the freshwater Alga Spirogyra and pollen of the freshwater Plant Myriophyllum alterniflorum. All of these species are indicative of freshwater ecosystems, but otherwise fairly cosmopolitan, and can be found in tropical and temperate environments.

Samples of pollen and spores were extracted from eight different cracks and holes on the surface of the stocks, with five samples being extracted from one large hole. A total of 7106 individual specimens were found, including 142 taxa of spores and pollen, from 18 trees, 21 shrubs, 91 herbs, 5 Ferns, and 7 types of Fungi, Algae, and Moss. This high proportion of herb pollen is likely to be indicative of an open agricultural environment, probably with low nutrient levels. This contained only a small proportion of Chenopodiaceaetype and Plantago maritima-type pollen, making a salt marsh environment unlikely. Many of the pollen types are cosmopolitan in distribution, but others, including Armeria, Cistaceae, Erica arborea, Lavandula, Nerium oleander, Olea, Pinus pinaster, Quercus ilex, Urtica pilulifera, Eryngium tenue, Corrigiola telephiifolia, and Vitis vinifera, are typical of the Mediterranean region, while others, including Erica australis, Erica umbellata, Cistus albidus, Cistus populifolius, Cistus ladanifer, and Halimium halimifolium, are found only on the western Iberian Peninsula and in western North Africa. Notably, the pollen of Cedrus and Chamaerops, which are more-or-less ubiquitous in recent North African sediments, were absent. 

Many pollen samples from cereal species showed signs of heat-deformation, something which has previously been observed in samples from medieval cesspits, and which is thought to be associated with bread or porridge-making.

The stocks also show signs of Insect damage in places, and yielded some Insect samples. The Insect damage comes in two forms. The first of these is wide flat tunnelling in the cambium layer, which would have underlain the bark, and which is caused by the larvae of Buprestid or Cerambycid Beetles. The second form of damage is a series of small boreholes likely to have been caused by Anobium punctatum, a small boring Beetle commonly associated with wooden beams and objects in Europe, which favours humid indoor environments. The Insect remains found belong to Ptinus fur or Ptinus clavipesAdistemia watsoniLatridius minutus, and two unidentified members of the Corticariinae. Adistemia watsoni is a species native to South America, but which had spread to Europe by the nineteenth century. The Spider Beetles, Ptinus fur and Ptinus clavipes, are typically found in indoor settings, feeding on Human food or other Pland and Animal remains. A small Mite belonging to the family Macrochelidae was also found. This assemblage has been found in other archaeological settings, and is considered typical of an indoor environment with mouldy food, litter and/or hay, and possibly excrement. 

The underside of one of the cross-braces, which is worn and shows traces of Fungal and Woodworm attack. Piena et al. (2024).

Artefacts will typically begin to assemble traces and small microparticles of biological origin from the moment when they are made, enabling researchers to build up a life history of  objects of interest. Examination of the assemblage associated with the Rijksmuseum stocks showed no evidence of these ever having visited South America, despite earlier interpretations.

A prior DNA analysis of the wood suggests that the stocks were made from a tree which probably grew somewhere between northern Spain and southern Scandinavia, and it seems unlikely that it was transported for any great distance before being worked. This is because only wood with a high market value is typically shipped for any great distance, which effectively means wood with a straight grain and few knots. The wood from which the stocks are made has an irregular grain pattern and is somewhat knotty, which would generally only be used if the desired task required wood to be sourced locally. The stocks also show signs of having been worked using techniques typical for green wood usage, which again makes it highly unlikely that the wood was transported any distance before being used.

The style of the stocks, with holes on top forcing the prisoner(s) to stand is unusual, but is known to have been used widely on the Iberian Peninsula during the early nineteenth century, leading Piena et al. to conclude that the stocks are likely to be of Iberian origin.

The samples collected can be expected to have started to accumulate as soon as the stocks were  made, and to have continued to accumulate throughout their existence. Samples were taken from locations all over the stocks, and in one in one location, a hole, a succession of samples were taken from different depths. Despite this, other than samples from the lower side being dusty and samples from the upper side being sandy, there was remarkably little difference in the samples, suggesting that the stocks spent much of their lives in a single environment. 

The pollen samples collected from the stocks suggest that this environment was in western Iberia, while the DNA collected from the wood suggests that it grew no  further south than northern Iberia, which is at least a neighbouring region. 

The Insects collected from the stocks suggest a humid, indoor environment, while the presence of cereal pollen, and good preservation of the Diatoms and pollen suggest that the sediment in which they were preserved did was not exposed to moisture for long periods.

Based upon this evidence, Piena et al. consider two separate scenarios, which could account for the accumulation of microfossils seen on the stocks. 

It is possible that the entire assemblage is post-use, representing a time when the stocks had been abandoned in a slow-moving stream or ditch, in an open agricultural environment with poor soils and intensive Rye cultivation, an environment typical of the Iberian Peninsula in the nineteenth century. This scenario is supported by the good preservation of pollen and Diatoms, the type of sediment found, and the low number of Fungal spores, but contradicted by the presence of sediment only on the upper side of the stocks, not on the underside or in the cavities between the beams and cross-braces. 

Alternatively, the large amount of pollen from wild Grasses and Cereals, particularly Rye, makes it possible that the stocks were used in an indoor environment where Grass and Rye straw were used as litter. This is supported by the types of spores present, which are all from species associated with decaying Plant matter or Animal dung (including Human). This is consistent with the idea that the stocks were used in a humid, indoor environment. The presence of Fungal and Woodworm damage to the underside of the stocks would be consistent with them sitting on a moist floor covered with a litter of straw and hay, possibly in a stable or dungeon (with the latter being more likely, given the presumed purpose of the stocks). Thus the deformed Cereal pollen could have come from bread or porridge fed to prisoners, or their faeces if they were forced to produce this while trapped in the stocks, and the sand in the cracks on the upper surface would be consistent with frequent scrubbing of this surface. 

Historically, most stocks around the world were positioned on their sides, with prisoners thus able to lie down. The Rijksmuseum stocks, however, are of a far rarer design, which held the prisoner in an upright position, forcing them to stand upright. Such stocks were often ued in conjunction with a neck brace on a wall, so that prisoners could be held upright and restrained. This was once common in Spanish prisons, providing a likely origin for the stocks. Notably, such stocks were particularly common during the Peninsula War of 1807-1814 and the Spanish War of Independence of 1814-1823, both wars which were noted for numerous attocities. In other settings, however, stocks of this type were combined with a latrine bench with holes, with prisoners being held in a sitting position.

Por liberal?, 1814–1823, by Francisco de Goya y Lucientes, showing a  woman trapped in a horizontal type of stocks. Piena et al. (2024).

When obtained, little was known about the set of stocks present in the collection of the Rijksmuseum. They were identified as having (recently) come from Zeeland, and were considered appropriate for an exhibition about the Dutch colony in Brazil between 1630 and 1658. Subsequent investigations have suggested that they were most likely made in Europe around 1800, and never taken to South America. Subsequent investigations by Piena et al. have narrowed the likely point of origin to the western Iberian Peninsula, and suggest that they were used in a moist indoor environment, most likely a dungeon.

See also...

Thursday, 9 May 2024

Three new species of Toktokkies from Southern Africa.

Toktokkies are Large Darkling Beetles from Southern Africa, which ger their common name from the distinctive noise they make by tapping their abdomens on the ground. They are stout, flightless Beetles with a chamber beneath the elytra where the wings were once found, used to trap moisture, which then drips down to the Insect's mouth where it can be drunk. This enables them to survive in arid environments such as the Namib Desert, where there are more than 20 species. The large an conspicuous nature of Toktokkies made them attractive to the zoological collectors of the nineteenth and twentieth centuries, resulting in many museums in Europe and North America amassing impressive collections. This is a problem for modern taxonomists, as the type specimens for described species are found in at least 59 institutions scattered around the world, making it hard to compare putative new species to all the species already described.

In a paper published in the journal Zootaxa on 29 April 2024, Marcin Jan Kamiński of the Museum  and  Institute  of  Zoology of the Polish Academy of Sciences describes three new species of Toktokkie from the Frey Beetle Collection at the Natural History Museum Basel, one of the world's largest collections of Darkling Beetles.

The first new species is placed in a new genus, Bouchardium, named in honour of Patrice Bouchard of the Canadian National Collection of Insects, Arachnids and Nematodes at Agriculture and Agri-Food Canada, and given the specific name chillygonzalesi, in honour of the Canadian pianist and composer, who goes by the stage name 'Chilly Gonzales'. The species is described on the basis of five specimens from Zimbabwe and Gauteng Province, South Africa.

Morphology of Bouchardium chillygonzalesi (holotype). Lateral (A), dorsal (B), posterior (C), and ventral (D) views of the body; prosternal process (E); epipleuron (F); label (G). Arrow indicates edge of epipleuron. Kamiński (2024).

Specimens of Bouchardium chillygonzalesi reach 20-24 mm in length, with a maximum elytral width of 10-13 mm. The head is prominent with downward-pointing mouthparts, the elytra high and domed. The body is dark brown, with the upper part of the elytra form a disk, also dark brown in colour, with a corrugated red border. The legs are covered by a dense coating of golden hairs.

The second new species is also placed in the genus Bouchardium, and is given the specific name mariae, in honour of Maria Antonina Kamińska, Marcin Jan Kamiński's daughter. The species is described on the basis of a number of specimens collected in Botswana, Gauteng Province (South Africa), Mozambique, and Zimbabwe.

Morphology of Bouchardium mariae (holotype and paratype). Lateral (A), dorsal (B), frontal (C), posterior (D), and ventral (E) views of the body; pronotum (F); prosternal process (G); label (H); aedeagal tegmen (I); spiculum gastrale (J). Kamiński (2024).

Specimens of Bouchardium mariae are 19-25 mm in length with the elytra having a maximum width of 12-14 mm. The head is prominent with downward-pointing mouthparts, the elytra high and domed. The body is black, with the upper part of the elytra form a disk, also black in colour, with a smooth red border. The legs are covered by a dense coating of golden hairs.

The third new species is placed in the genus Toktokkus, and given the specific name zofiae, in honour of Zofia Irena Kamińska, also Marcin Jan Kamiński's daughter. This species is described on the basis of a single specimen from Gemsbok Pan, in North West Province, South Africa. 

Morphology of Toktokkus zofiae (holotype) (A–F) and T. herero (G, H). Lateral (A), dorsal (B), and ventral (C) views of the body; pronotal disc (D), prosternal process (E, H); label (F); and elytral disc (G). Kamiński (2024).

The single known specimen of Toktokkus zofiae is 18.5 mm long with a maximum elytral width of 11.0 mm. I he head is prominent with downward-pointing mouthparts, the elytra relatively flattened with flanks covered in microtubercles. The legs are covered by a dense coating of golden hairs.

See also...

Saturday, 6 April 2024

Cretafrica orapensis: A new species of Mycetoporine Rove Beetle from the Cretaceous Orapa Diamond Mine deposits of Botswana.

Rove Beetles, Staphylinidae, are considered to be the most specious group of Animals alive today, with 66 928 described species in 35 subfamilies. The group appeared around the beginning of the Jurassic, with the majority of the extant subfamilies having appeared by the end of that period, and with significant ongoing diversification through the Cretaceous. The subfamily Mycetoporinae contains about 444 described species in 16 genera. It has a rather limited fossil record, with four known species from the Early Cretaceous of Russia and China, Cuneocharis elongata and Ryvkinius gracilis from the Daya Formation, and Undiatina pilosa from the Semyon Formation, all from Russia, and Glabrimycetoporus amoenus from the Yixian Formation of China, and several specimens assigned to the genera Lordithon and Mycetoporus from the Eocene Florissant Formation of the United States.

In a paper published in the journal Insect Systematics & Evolution on 29 March 2024, Sandiso Mnguni of the Evolutionary Studies Institute and Centre of Excellence in Palaeosciences at the University of the Witwatersrand, and Ian James McKay and Shaw Badenhorst, also of the School of Geosciences at the University of the Witwatersrand, describe a new species of Mycetoporine Rove Beetle from the Cretaceous Orapa Diamond Mine deposits of Botswana.

The Opara Diamond mine exploits two diamondiferous kimberlite pipes, (igneous deposits in which material from deep within the Earth is extruded upwards though existing deposits) which cut through Late Cretaceous deposits, reaching the surface and forming a volcanic crater in the Turonian, about 93.1 million years ago. Mining operations here have formed a large oval pit, which, as well as the kimberlite pipes, has exposed a series of lacustrine sediments preserving fossil Plants and Insects.

A top view of the Orapa Diamond Mine showing the open pit left after the removal of the crater lake facies and kimberlite. June 2018. Ian James McKay in Mnguni et al. (2024).

The new species is given the name Cretafrica orapensis, where 'Cretafrica' is a combination of Cretaceous and Africa, and 'orapensis' means 'from Orapa'; Orapa itself means 'the resting place of Lions' in the Sesarwa language, a name originally given to a cattle post near the site where diamonds were discovered. The species is described from a single specimen, a well-preserved impression fossil, and both dorsal and ventral structures are superimposed, and thus visible on top of each other. A second, smaller Beetle is also preserved on the same slab, which is probably a Hydroscaphid Water Beetle.

The whole body of Cretafrica orapensis, holotype, BP./2/27480, Orapa Diamond Mine, nonpolarised light, scale bar is 1mm. Abbreviations: e, eye; h, hypomeron; ek, epipleural keel; ef, epipleural fold; ppt, paired paratergite; spt, single paratergite; ss, spiral structure. Mnguni et al. (2024).

The specimen is 4.92 mm long and 1.58 mm wide.  The head is elongated and triangular, with small oval eyes towards the rear. The antennae are poorly preserved, but probably have eleven segments and were located anterior to the eyes. Mandibles, maxillary and maxillary palps are visible, but poorly preserved. The pronotum (forepart of the thorax) is hard to interpret, as it is partially covered by sediment. The Elytra cover less than a third of the body, leaving six abdominal segments exposed. 

Finding a member of the Mycetoporinae at Orapa has significant implications for the history of the group. Four previous Lower Cretaceous specimens have been described from three different localities, though these were all on the eastern part of the Eurasian landmass. The discovery of a specimen from Southern Africa, significantly increases the geographical range of Early Cretaceous Mycetoporine Rove Beetles, indicating that the group must have been in existence for long enough to achieve a near global distribution by this time.

Global palaeogeographic reconstruction of the mid-Cretaceous (100 million years ago) showing the localities where fossil Mycetoporinae have been recovered. Abbreviations: Ob, Obeschayushchiy locality (Daya Formation), Russia; Se, Semyon Formation, Russia; Yi, Yixian Formation, China; and Or, Orapa, Botswana. Mnguni et al. (2024).

See also...

Tuesday, 26 March 2024

Paleothius mckayi: A new species of Rove Beetle from the Late Cretaceous of Botswana.

Rove Beetles, Staphylinidae, are considered to be the most specious group of Animals alive today, with 66 928 described species in 35 subfamilies. The group appeared around the beginning of the Jurassic, with the majority of the extant subfamilies having appeared by the end of that period, and with significant ongoing diversification through the Cretaceous. The subfamily Staphylininae contains 9071 described species in 411 genera, making it the third most diverse subfamilies of Rove Beetles, behind the Aleocharinae and Pselaphinae. The Staphylininae is in turn divided into eight extant tribes, the Arrowinini, Coomaniini, Diochini, Maorothiini, Othiini, Platyprosopini, Staphylinini, and Xantholinini, as well as the extinct Thayeralinini. The oldest Staphylinines, Tunicopterus sigara and Subcelytrinus antiquus from the Karatau Formation of Kazakhstan; and Sinostaphylius xiejiajieensis from the Jiuda Formation in China date from the Jurassic, with a further 27 species described from the Cretaceous, and 57 from the Cainozoic. 

In a paper published in the Journal of Entomological Science on 4 March 2024, Sandiso Mnguni of the Evolutionary Studies Institute and the Centre of Excellence in Palaeosciences at the University of the Witwatersrand, and Shaw Badenhorst, and Marion Kathleen Bamford, also of the Evolutionary Studies Institute at the University of the Witwatersrand, describe a new species of Staphylinine Beetle from the Cretaceous deposits of the Orapa Diamond Mine in Botswana.

The Opara Diamond mine exploits two diamondiferous kimberlite pipes, (igneous deposits in which material from deep within the Earth is extruded upwards though existing deposits) which cut through Late Cretaceous deposits, reaching the surface and forming a volcanic crater in the Turonian, about 93.1 million years ago. Mining operations here have formed a large oval pit, which, as well as the kimberlite pipes, has exposed a series of lacustrine sediments preserving fossil Plants and Insects.

A top view of the Orapa Diamond Mine showing the open pit left after the removal of the crater lake facies and kimberlite. June 2018. Ian James McKay in Mnguni et al. (2024).

The new species is placed in the genus Paleothius, which currently contains a single species, Paleothius gracilis from the Early Cretaceous of China, and is given the specific name Paleothius mckayi, in honour of  Ian James McKay (1963–2022), who was a palaeoentomologist and Geosciences Outreach Education Specialist at the University of the Witwatersrand, Johannesburg, South Africa, who spent many years describing fossil insects from the Orapa Diamond Mine, and also trained various undergraduate and postgraduate students, including Sandiso Mnguni, who went on to become the first black palaeoentomologist in South Africa.

The whole body of Paleothius mckayi, holotype, Orapa Diamond Mine, polarised light. Mnguni et al. (2024).

Paleothius mckayi is a narrow, slender and cylindrical Rove Beetle, measuring 7.70 mm in length (from tip of mandibles to tip of abdomen) and 0.80 mm in width (from exterior edge of left elytron to edge of right elytron). The last abdominal segment is seemingly covered with setae.

Paleothius mckayi is the first fossil Staphylinine Beetle from Africa, and the first from the Southern Hemisphere, with previous Cretaceous Staphylinine Beetles known from China, Myannmar, Russia, and the UK. This makes Botswana a significant extension to the range of the group at this time, though perhaps not a surprising one; the Staphylininae are estimated to have split from their sister group, the Paederinae in the Late Jurassic, about 156.6 million years ago (other estimates put the split between 180 and 145 million years ago), and a Paederine Rove Beetle has previously been discovered from the Orapa deposits. 

Global palaeogeographic reconstruction of the mid-Cretaceous (100 million years ago) showing the localities where the fossil Staphylininae have been recovered. Abbreviations: Bu, Burmese Amber, Myanmar; La, Laiyang Formation, China; Or, Orapa Diamond Mine, Botswana; Yi, Yixian Formation, China; Ma, Magadanskaia, Russia and Lu, Lulworth Formation, Middle Purbeck, UK. Mnguni et al. (2024).

See also...

Friday, 1 March 2024

Bityle oriens: A new species of Longhorn Beetle from Mindanao Island, the Philippines.

The islands of the Philippines are considered to be one of the world's biodiversity hotspots, with a largely tropical forest ecosystem scattered across a large number of islands, leading to a very high rate of endemism (the occurrence of species with limited geographical ranges). However, much of this biodiversity is currently threatened by habitat loss as forests are converted to agricultural use. One of the groups most threatened by this are Beetles, a hyper-diverse Insect group which reach their most specious in tropical forests. Many Beetles found in the Philippines are unique to the islands, but often closely related to species found in Indonesia, Malaysia, and elsewhere in Southeast Asia.

In a paper published in the Philippine Journal of Science in February 2024, Milton Norman Medina of the Tropical Genomics Laboratory and the Faculty of Agriculture and Life Sciences at Davao Oriental State University, and the National Museum of Natural History Philippines, Amy Ponce, also of the Faculty of Agriculture and Life Sciences at Davao Oriental State University, and Jhonnel Villegas of the Faculty of Teacher Education and Center for Futures Thinking and Regenerative Development at Davao Oriental State University describe a new species of Longhorn Beetle from Davao Oriental Province on Mindanao Island, the Philippines.

The new species is placed in the genus Bityle, which contains six previously described species from Mindanao and Luzon islands in the Philippines and Sulawesi in Indonesia, and given the specific name oriens, meaning 'east', in reference to Davao Oriental Province. The species is described from one male and two female specimens collected in the Municipality of Boston, which is part of the Eastern Mindanao Biodiversity Corridor, a continuous stretch of forest ecosystems that serve as a biological sanctuary in the eastern part of Mindanao.

Habitus of Bityle oriens: (A) Holotype male, dorsal aspect; (B) paratype female, dorsal aspect; (C) frons of male holotype; (D) lateral aspect, male holotype. Medina et al. (2024).

Females of Bityle oriens are slightly larger than males, reaching 9.5 mm as opposed to 8.0 mm, but otherwise externally similar. The Beetles are black in colour, with white hairs on the head, antennae, legs, and underside, while the upper part of the body is covered by black hairs, except three bands of white hairs on the elytra.

See also...