Showing posts with label Eurasia. Show all posts
Showing posts with label Eurasia. Show all posts

Sunday, 7 May 2023

Human DNA extracted from a Palaeolithic pendant.

Understanding the changes in technology and population that went on during the Palaeolithic is the key to understanding much of the history of our species. Unfortunately, Palaeolithic deposits tend to be highly condensed, so that objects and remains found alongside one-another may be separated by hundreds or even thousands and years, making it impossible to connect artefacts to remains unless they were clearly directly buried together. 

Recent advances in the recovery of DNA from ancient sediments provide us with the possibility of establish connections between artefacts and specific Human populations, although this would require the recovery of DNA directly from the objects in question. Potentially, artefacts made from tooth and bone have the best chance of preserving ancient DNA, as they are porous and capable of absorbing body fluids, and because they contain hydroxyapatite, which is known to both absorb and preserve DNA. Thus ancient pieces of tooth or bone may potentially preserve DNA not only from the Animal from which they came, but also DNA from other organisms that came into contact with them after that Animal's death, For the most part, this tends to be the DNA of Microorganisms which colonised the decaying body of the original Animal, but could also potentially include Humans which handled these pieces, or made things from them. 

However, Palaeolithic artefacts made from tooth and bone are extremely rare, and therefore of great value to science, something particularly true of pendants or other objects likely to have been worn close to the skin for long periods of time, and therefore the most likely to have absorbed ancient Human DNA. The conservation of such objects is therefore considered a high priority, and archaeologists are reluctant to expose them to the destructive methods used to extract DNA, or even to soak them in buffers which might absorb DNA passively, as these can alter specimens irreparably. 

In a paper published in the journal Nature on 3 May 2023, a team of scientists led by Elena Essel of the Max Planck Institute for Evolutionary Anthropology, Elena Zavala, also of the Max Planck Institute for Evolutionary Anthropology, and of the Department of Biology at San Francisco State University, and the Department of Molecular and Cell Biology at the University of California, BerkeleyEllen Schulz-Kornas of the Department of Cariology, Endodontology and Periodontology at the University of Leipzig, Marie Soressi of the Faculty of Archaeology at Leiden University, and Matthias Meyer, again of the Max Planck Institute for Evolutionary Anthropology, describe development of a method for non-destructively recovering DNA from ancient bone and tooth artefacts, and the first results obtained using this technique.

In order to test potential reagents for DNA extraction from ancient artefacts, Essel et al. first obtained ten pieces of faunal remains from the  Quinçay and Les Cottés Palaeolithic sites in France, none of which are thought to have been deliberately modified by Human activity, but all of which were similar in size and shape to common bone and tooth artefacts. These were immersed in ten different potential reagents, including a guanidinium thiocyanate-containing reagent previously suggested for non-destructive DNA extraction, an ethylenediaminetetraacetate (EDTA) solution, which is a decalcifier commonly used in ancient DNA extraction,  a sodium hypochlorite (bleach) solution, which is an oxidizing reagent used to remove surface-exposed contaminant DNA, and a sodium phosphate buffer supplemented with detergent, which has been recently shown to enable temperature-controlled DNA release from powdered bone samples.

The microtopography of the surface of these artefacts was mapped  using quantitative 3D surface texture analysis prior to immersion, and then again once the samples were removed, in order to detect any changes caused by the reagents. The guanidinium thiocyanate-containing reagent and ethylenediaminetetraacetate solution were both found to cause significant alteration to the samples, whereas all of the other samples caused much smaller and more sporadic changes (none of the reagents caused zero alterations), possibly due to the removal of small particles of soil and other substances from the sample surfaces. 

Faunal remains used in reagent testing. Photographs of samples taken before and after treatment with various reagents used in ancient DNA extraction (GuSCN, guanidine thiocyanate reagent; EDTA, ethylenediaminetetraacetate solution; Phosphate, sodium phosphate buffer with detergent; Bleach, sodium hypochlorite solution). The black bar represents 1 cm. Note that colours are not directly comparable, as the photographs were taken at slightly different angles, with different light settings and camera adjustments. Essel et al. (2023).

Based upon this, Essel et al. were able to develop a step-wise method for the extraction of DNA from ancient bone and tooth artefacts. using serial incubations in sodium phosphate buffer at 21, 37, 60 and 90 °C, with three incubations per temperature.

Workflow of the gradual, non-destructive DNA extraction method using sodium phosphate buffer at elevated temperatures. Essel et al. (2023).

Next Essel et al. applied this to eleven bone and tooth objects from Châtelperronian layers of Quinçay Cave in France, all of which are believed to have potentially been used as tools between 35 000 and 45 000 years ago. One of these objects (Q10), identified as a piece of Reindeer bone, yielded 1828 fragments of Cervid mitochondrial DNA, which showed elevated frequencies of cytosine-to-thymine substitutions at their ends, which is consistent with the deamination of cytosine seen in other ancient DNA samples, and which has been used to date such DNA. Another object (Q15), identified as a piece of ivory, yielded 2004 fragments of Elephantid mitochondrial DNA, again showing cytosine-to-thymine substitutions. All eleven samples also yielded Hominid and Suid mitochondrial DNA, none of which showed cytosine-to-thymine substitutions, and all of which is therefore is considered to be the result of modern contamination. Since all of these samples were found several decades ago, and were neither collected or stored under sterile conditions, this was not surprising.

Artefacts before and after DNA extraction. Photographs of samples taken before and after phosphate-based, non-destructive DNA extraction. The black bar represents 1 cm. Note that colors are not directly comparable, as the photographs were taken at slightly different angles, with different light settings and camera adjustments. Essel et al. (2023).

Given that contamination by modern DNA appeared to be ubiquitous in ancient bone and tooth objects that had been handled by hand, Essel et al. decided to directly obtain objects from ongoing excavations at two Palaeolithic sites currently still under investigation; Bacho Kiro Cave in Bulgaria, and Denisova Cave in the Altai Republic of southern Siberia. Three tooth pendants (‘BKP1–BKP3) were obtained from Bacho Kiro, and one (DCP1) from Denisova Cave, all by archaeologists wearing gloves and facemasks to prevent contamination.

Photograph of DCP1 as it became exposed during excavation. The photograph was taken shortly before the pendant was removed and placed into a plastic bag using gloves. Essel et al. (2023).

Large and visible chunks of soil were removed from these artifacts by (gloved) hand, and they were washed in water three times before being subjected to the phosphate buffer DNA extraction technique. All four pendants produced ancient Mammalian mitochondrial DNA, with BKP1 producing Bovid DNA, BKP2 and BKP3 producing Ursid DNA, and DCP1 producing Cervid DNA. Human mitochondrial DNA was recovered at much lower levels than from the Quinçay material, and very few pieces of Suid DNA suggesting that the modified excavation method had helped prevent the contamination of these samples. Notably, the DCP1 Human mitochondrial DNA showed signs of significant cytosine deamination, suggesting that this was indeed ancient Human DNA.

Photographs of DCP1 before and after cleaning and non-destructive DNA extraction. Essel et al. (2023).

Very little ancient Human mitochondrial DNA was recovered from the Bacho Kiro Cave material, with the largest sample, 29 deaminated fragments, coming from a soil particle attached to BKP3. In contrast, DCP1 produced significant amounts of ancient Human mitochondrial DNA, enabling the construction of a near-complete consensus sequence, which could be used to place the material within a phylogenetic analysis. This DNA seemed to mostly (but not exclusively) originate from a single individual, assigned to mitochondrial haplogroup U (because mitochondrial DNA is found in the mitochondria, organelles outside the cell nucleus, it is passed directly from mother to child without being sexually recombined each generation, enabling precise estimations of when individuals shared common ancestors, at least through the female line, forming a mitochondrial  haplogroup).

Essel et al. estimate that this Human mitochondrial DNA came from an individual lived about 18 500 years ago, and falls within a group of Ancient North Eurasians who otherwise are known from further east within Siberia, including the 24 000-year-old Mal’ta 1 individual, and the 17 000-year-old Afontova Gora 3 individuals. All of these samples are more closely related to one-another than to modern North Eurasians, and show affinities to other ancient Siberians and Native Americans. As well as the mitochondrial DNA, sufficient chromosomal DNA was recovered to establish that the individual was female.

Essel et al.'s work establishes that it is possible to recover ancient Human DNA from bone and tooth artefacts, providing a previously unexplored source of information about the makers and users of these ancient objects. The amount of ancient DNA recovered from DCP1 was comparable to that obtained from well-preserved Pleistocene Human remains, and the recovery of both Human and Cervid DNA from the same object enabled two separate cytosine deamination dates from the same artefact.

Future work will determine how frequently such ancient Human DNA is preserved within bone and took artefacts. Essel et al. recommend that all archaeologists working with such material adopt the practice of wearing gloves and masks while extracting bone and tooth sample at archaeological sites, and express the hope that in future it might be possible to establish a dataset which can connect specific late Pleistocene technologies to specific ancient Human populations.

See also...

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Thursday, 6 August 2015

Cryptic diversity: A new species of Wolf from Africa.


Cryptic species are species which closely resemble other species and which can only be separated by careful anatomical examination or even genetic analysis. In recent years the widespread application of DNA analysis to populations of wild animals  has led to the discovery that many well-known species are in fact clusters of cryptic species, with profound implications for the conservation of these species; a single large widespread population suddenly becoming a number of smaller more localized populations. 

Golden Jackals, Canis aureus, from North Africa have long been noted for being larger and more robust than Jackals from either Sub-Saharan Africa or Eurasia, leading to speculation that they may represent a separate species or sub-species. A study published in 2011 in the journal PLoS One based upon analysis of mitochondrial DNA found that Jackals from Egypt and Ethiopia were in fact not Jackals at all, but were more closely related to the Grey Wolf, Canis lupus, and suggested that these should be described as a separate subspecies of Wolf, the African Wolf, Canis lupus lupaster. A follow-up study published in the same journal in 2012 found that the mitochondrial lineage ascribed to Canis lupus lupaster was also present in Canids in West Africa, among animals considered to be more typically Jackal-like.

In a paper published in the journal Current Biology on 17 August 2015, a team of biologists led by Klaus-Peter Koepfli of the Smithsonian Conservation Biology Institute and the Theodosius Dobzhansky Center for Genome Bioinformatics at St. Petersburg State University and John Pollinger of the Department of Ecology and Evolutionary Biology at the University of California, Los Angeles publish the results of a much wider study of mitochondrial and nuclear DNA from populations of Golden Jackals from across Southern Europe and the Middle East, as well as Israel, Morocco, Algeria, Mauritania, Senegal and Kenya, and discusses these results and their implications for the classification of African Jackals.

All of the African Jackals were found to be a separate species from the Eurasian Jackals, and more closely related to the Eurasian Grey Wolf. However these African Wolves appear to have separated from their Eurasian cousins over a million years ago, and were judges sufficiently genetically distinct to be placed in a separate species. Examination of taxonomic records for Canids revealed that the French biologist Cuvier had described a ‘Jackal’ from Senegal as a separate species, Canis anthus, in 1820, an analysis that was rejected by subsequent biologists who failed to spot any significant morphological difference between African and Eurasian Jackals. For this reason Koepfli & Pollinger et al. suggest that African Golden Jackals henceforth be referred to as African Golden Wolves, Canis anthus, rejecting Canis lupus lupaster as a valid name.

Phylogenetic Tree Based on Mitochondrial Cytochrome b Sequences and Sampling Localities of Golden Jackals Used in This Study (A) Maximum-likelihood phylogram of 104 cytochrome b sequences (1,140 bp). Haplotype number is shown next to taxon name and locality. Accession numbers indicate sequences downloaded from GenBank. Haplotypes without accession numbers are novel sequences generated for the present study. Asterisks at nodes indicate bootstrap support R80% based on maximum-likelihood analyses (500 pseudoreplicates) and R0.95 posterior probability from Bayesian inference. Canis spp. from Egypt are indicated by thick arrows. Haplotypes labeled as Canis lupus lupaster refer to the African wolf. The tree was rooted using Sechuran Fox (Lycalopex sechurae) as outgroup. Scale bar indicates the number of substitutions per site. Photo credits: left, Golden Jackal from Senegal (CIBIO/Monia Nakamura); centre, Mexican Gray Wolf (Tom and Pat Leeson); right, Golden Jackal from Israel (Eyal Cohen). (B) Map of geographic localities showing where Golden Jackals were sampled. Relative number of animals sampled from each locality is shown. Hatched lines indicates geographic range of Golden Jackal based on International Union for the Conservation of Nature distribution. Koepfli & Pollinger et al. (2015).

Morphologically the African Golden Wolf and Eurasian Golden Jackal are very hard to tell apart, other than the distinct largeness of the North African specimens; the African Wolf was, on average slightly broader in the snout than the Eurasian Jackal, but not distinctively enough for this to be used as a reliable feature to distinguish the species.

The Golden Jackal samples from Israel were found to be mostly hybrid animals, containing DNA from Eurasian Golden Jackals, Grey Wolves, African Golden Wolves and Dogs. Two Golden Wolves from Egypt were found to have mitochondrial DNA (which is passed through the female line without recombination) from Eurasian Jackals and Grey Wolves, suggesting that hybridization was occurring here too, though whole genome analysis of Egyptian samples was not carried out.

Comparison of the genomes of African Golden Wolves and Dogs suggest that a small amount of Dog DNA derives from African, rather than Grey Wolves; this is roughly comparable to the amount of Neanderthal DNA found in modern Humans, with two groups of Dogs, the Basanji (African Laughing Dog) and Dingo, having higher levels of Golden Wolf DNA than other groups.

This scenario suggests that Africa has repeatedly been invaded by different Canid lineages from Eurasia. Koepfli & Pollinger et al. suggest that this relates to the changeable climate of the Pleistocene Era, with warmer wetter periods when it was possible for Canids to move between Eurasia and Africa, and cooler dryer periods when these populations became reproductively isolated.

See also…

Morphometric analysis is a method used by palaeontologists to sort bones and shells into taxonomic and ecological groups. It relies...


Foxes (Vulpini) are a subgroup of the Dog Family, Canidae, found in North America, Eurasia and Africa (South American Foxes are a separate group, more closely related to True Dogs than to other Foxes). The...


Dogs are our oldest domestic animal, and the only one which predates the adoption of agriculture. This has led to a great deal of study of the origin of domestic dogs over the years. Despite this we are still not entirely sure where dogs were first domesticated. We are now confident that domestic dogs are descended from a...



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Friday, 12 September 2014

Magnitude 1.9 Earthquake in North Yorkshire.

The British Geological Survey recorded a Magnitude 1.9 Earthquake at a depth of 1 km in southern North Yorkshire slightly after 11.30 pm British Summertime (sightly after 10.30 pm GMT) on Thursday 11 September 2014. This is quite a small quake, and there was no danger of it causing any damage or injuries, but it people have reported feeling it in parts of North and East Yorkshire.

The approximate location of the 11 September 2014 North Yorkshire Earthquake. Google Maps.

Earthquakes become more common as you travel north and west in Great Britain, with the west coast of Scotland being the most quake-prone part of the island and the northwest of Wales being more prone  to quakes than the rest of Wales or most of England.

The precise cause of Earthquakes in the UK can be hard to determine; the country is not close to any obvious single cause of such activity such as a plate margin, but is subject to tectonic pressures from several different sources, with most quakes probably being the result of the interplay between these forces.

Britain is being pushed to the east by the expansion of the Atlantic Ocean and to the north by the impact of Africa into Europe from the south. It is also affected by lesser areas of tectonic spreading beneath the North Sea, Rhine Valley and Bay of Biscay. Finally the country is subject to glacial rebound; until about 10 000 years ago much of the north of the country was covered by a thick layer of glacial ice (this is believed to have been thickest on the west coast of Scotland), pushing the rocks of the British lithosphere down into the underlying mantle. This ice is now gone, and the rocks are springing (slowly) back into their original position, causing the occasional Earthquake in the process. 

(Top) Simplified diagram showing principle of glacial rebound. Wikipedia. (Bottom) Map showing the rate of glacial rebound in various parts of the UK. Note that some parts of England and Wales show negative values, these areas are being pushed down slightly by uplift in Scotland, as the entire landmass is quite rigid and acts a bit like a see-saw. Climate North East.

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. If you felt this quake, or were in the area but did not (which is also useful information) then you can report it to the British Geological Survey here.

See also...


The British Geological Survey recorded a Magnitude 1.7 Earthquake at a depth of 1 km, roughly 5 km to the west...


A Magnitude 1.9 Earthquake occurred at a depth of about 1 km roughly 10 km to the east of Doncaster in South Yorkshire, slightly after 4.50 am British...



On Wednesday 23 May at about 10.45 pm British Summertime (11.45 GMT), the British Geological Survey recorded an Earthquake in South Yourkshire, roughly 3 km west of the Village of Thorne, or 10 northeast of Doncaster, measuring 1.4 on the Richter Scale and at a depth of 1 km. This is a very small quake and is highly unlikely to have caused any damage or injuries, but may have been felt as it was close to the surface.




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Friday, 4 July 2014

Magnitude 2.9 Earthquake near Fort William, Scotland.

The British Geological Survey recorded a Magnitude 2.9 Earthquake at a depth of 5 km roughly 10 km to the west of Fort William in Highland County, Scotland, slightly after 7.35 pm British Summertime (slightly after 6.35 pm GMT) on Thursday 3 July 2014. This is a large quake for Scotland, but not dangerous and there are no reports of any damage or casualties, though the quake was felt across much of the Highland region.

Map showing areas where people reported feeling the 3 July 2013 quake. British Geological Survey.

Earthquakes become more common as you travel north and west in Great Britain, with the west coast of Scotland being the most quake-prone part of the island and the northwest of Wales being more prone  to quakes than the rest of Wales or most of England.

The precise cause of Earthquakes in the UK can be hard to determine; the country is not close to any obvious single cause of such activity such as a plate margin, but is subject to tectonic pressures from several different sources, with most quakes probably being the result of the interplay between these forces.

Britain is being pushed to the east by the expansion of the Atlantic Ocean and to the north by the impact of Africa into Europe from the south. It is also affected by lesser areas of tectonic spreading beneath the North Sea, Rhine Valley and Bay of Biscay. Finally the country is subject to glacial rebound; until about 10 000 years ago much of the north of the country was covered by a thick layer of glacial ice (this is believed to have been thickest on the west coast of Scotland), pushing the rocks of the British lithosphere down into the underlying mantle. This ice is now gone, and the rocks are springing (slowly) back into their original position, causing the occasional Earthquake in the process. 

(Top) Simplified diagram showing principle of glacial rebound. Wikipedia. (Bottom) Map showing the rate of glacial rebound in various parts of the UK. Note that some parts of England and Wales show negative values, these areas are being pushed down slightly by uplift in Scotland, as the entire landmass is quite rigid and acts a bit like a see-saw. Climate North East.

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. If you felt this quake, or were in the area but did not (which is also useful information) then you can report it to the British Geological Survey here.

See also...


The British Geological Survey recored a Magnitude 1.3 Earthquake at a depth of 7 km on the Ardnamurchan Peninsula in the...



The British Geological Survey recorded a Magnitude 1.4 Earthquake at a depth of 2 km in the Torridon Hills of western Ross and...



The British Geological Survey recorded a Magnitude 2.4 Earthquake at a depth of 2 km in the Highlands of Scotland, on the west bank...


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Monday, 17 March 2014

An American Hyaenodontid in China.

The Hyaenodontidae were a group of carnivorous Mammals the appeared in the the Late Palaeocene and continued till the Late Miocene. Their name means 'Hyena-toothed', though they are not closely related to the Hyenas, or any other extant Mammal group. They were formerly classified with the Oxyaenids in a group called the Creodonts, though that group is now thought to be polyphyletic; i.e. the two groups which formerly were classified together to form the Creodonts are no longer thought to be closely related.

In a paper published in the journal Palaeontology in January 2014, Michael Morlo of the Forschungsinstitut SenckenbergKatharina Bastl of the Institut für Paläontologie and the Forschungsgruppe Aerobiologie und Polleninformation at Universität Wien, Wu Wenhao of the  Research Center of Palaeontology at Jilin University and Stephan Schaal, also of the Forschungsinstitut Senckenberg, describe a new species of Hyaenodontid from the late middle Eocene Huadian Formation of Jilin Province China.

The new species is placed in the genus Sinopa, and given the specific name jilinia, meaning ‘from Jilin’. The species is described from a right dentary (jawbone) preserved in two fragments, recovered from the Gonglangtou Coal Mine in Jilin Province.

Right dentary of Sinopa jilinia from Gonglangtou, late middle Eocene. (A) labial view, (B) occlusal view, (C) lingual view of the main part of the right hemimandible with m1–3, (D) labial view, (E) lingual view, (F) occlusal view of the smaller fragment of the right hemimandible with p2–p3. Note m3 smaller than m1, backward leaning protoconids, very labially postvallid origin of cristid obliquum and continuous labial cingulids in all molars. Morlo et al. (2014).

The genus Sinopa has previously been described only from North America; this is its first occurrence in Asia. The presence of Hyenadontids in China is not unexpected; the group is believed to have arisen in Africa, and spread through Eurasia to North America by the early Eocene, however the genus Sinopa is thought to have arisen in North America, after faunal interchange with eastern Asia had largely ceased. The presence of Sinopa jilinia in northeast China adds to a small, but growing, body of evidence that faunal interchange between Asia and North America may have persisted for longer than previously thought. 


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Wednesday, 4 September 2013

Magnitude 1.7 Earthquake in Argyll & Bute, Scotland.

The British Geological Survey recorded a Magnitude 1.7 Earthquake at a depth of 2 km, roughly 5 km to the southwest of Ben Lui in Argyll and Bute, Scotland, slightly before 7.45 am British Summertime (slightly before 6.45 am GMT) on Tuesday 3 September 2013. This is not a large quake, and is unlikely to have caused any damage or casualties, though it may have been felt locally.

The approximate location of the 3 September 2013 Argyll & Bute Earthquake. Google Maps.

As a rough rule of thumb, when you travel further to the north and west in Great Britain Earthquakes become more frequent, making Scotland (in particular western Scotland) the most quake prone area of the country. The precise causes of British Earthquakes can be hard to determine, as the country is not close to any active plate boundary, but is subject to tectonic stresses from a number of different sources.

Scotland (along with the rest of Eurasia) is being pushed to the east by the expansion of the Atlantic Ocean and to the north by the impact of Africa into Europe from the South. Closer to home there are lesser centers of expansion beneath the North Sea, the Rhine Valley and the Bay of Biscay, all of which excerpt pressure on Scottish rocks. Finally there is glacial rebound; until about 10 000 years ago much of the UK was covered by a thick layer of ice, pushing the rocks of the lithosphere down into the underlying mantle; this ice is now gone and the rocks are (slowly) rebounding, causing the occasional Earthquake in the process.

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. If you felt this quake, or were in the area but did not (which is also useful information) then you can report it to the British Geological Survey here.


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Tuesday, 19 March 2013

Earthquake in Norfolk.

On Saturday 16 March 2013, slightly after 7.00 am GMT, the British Geological Survey recorded a Magnitude 2.1 Earthquake in Norfolk, roughly 30 km southwest of Norwich, at a depth of 4 km. This is not a large enough magnitude to have caused any serious damage, but it is large enough that it may have been felt locally.

The location of the 16 March 2013 Earthquake. Google Maps.

The precise cause of earthquakes in the UK can be hard to determine. The country is not located close to any single large source of tectonic activity, so that most quakes are probably the result of the interaction of a number of stresses. 

Britain (along with the rest of Eurasia) is being pushed to the east by the expansion of the Atlantic Ocean, and to the north by the impact of Africa into Europe from the south. There are also smaller but more local centers of tectonic expansion beneath the North Sea, Rhine Valley and Bay of Biscay, all of which exert some stress upon rocks in the UK. Finally there is glacial rebound; until about 10 000 years ago much of the north of the UK was covered by a thick layer of glacial ice, which pushed the rocks of the lithosphere down into the underlying mantle. This ice is now gone, and the rocks are slowly springing back into there original position, causing the occasional Earthquake in the process.

Witness reports of Earthquakes can help scientists to understand these events, and the underlying geologic processes that cause them. If you felt this quake (or were in the are but did not, which is also useful information), then you can report it to the British Geological Survey here.


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Saturday, 12 January 2013

Earthquake in northern Nottinghamshire.

On Saturday 12 January 2013, slightly before 4.00 am, GMT, the British Geological Survey recorded a Magnitude 1.3 Earthquake 1 km beneath northern Nottinghamshire, England, roughly 2 km southwest of the village of Ollerton, or 10 km northeast of the town of Mansfield. This is to small a quake to have caused any damage, but it was felt in the villages of Ollerton and Walesby.

The location of the 12 January 2013 Earthquake. Google Maps.

The UK is not close to any active plate margin, and it is seldom possible to point to a single cause for any Earthquake there. Rather most quakes are the result of a combination of several different tectonic pressures interacting. Britain, along with the rest of Eurasia, is being pushed to the east by the expansion of the Atlantic Ocean and to the north by the impact of Africa into Europe from the south. There are also lesser areas of expansion beneath the North Sea, the Rhine Valley and the Bay of Biscay, all of which exert pressure on British rocks. Finally there is glacial rebound; much of the north of Britain was covered by a thick layer of glacial ice until about 10 000 years ago. This pushed the rocks of the British lithosphere down into the underlying mantle. This ice is now gone, and the rocks of the lithosphere are now springing back into position (at geological speeds) causing the occasional Earthquake in the process.

Witness accounts can help geologists to understand Earthquakes and the geological structures that lead to them. If you felt this quake (or were in the area but did not, which is also useful information) then you can report it to the British Geological Survey here.


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Thursday, 10 January 2013

Earthquake in southern Spain.

On Thursday 10 January 2012, slightly before 12.30 am local time (slightly before 11.30 pm on Wednesday 9 January 2012, GMT), the United States Geological Survey recorded a Magnitude 3.5 Earthquake, at a depth of 21 km, beneath souther Spain, roughly 30 km northwest of Granada. This is not large enough to have caused any serious damage, though it was reportedly felt across a fairly wide area.

The location of the 10 January Earthquake. Google Maps.

Iberia is located on the extreme southwest of the Eurasian Plate, close to the margin with Africa, which is pushing into Europe from the south. At the same time there is a lesser area of geological expansion beneath the Bay of Biscay, pushing Iberia southwards. This leads to considerable tectonic stress in southern Spain, leading in turn to the occasional Earthquake.


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Sunday, 30 December 2012

Earthquake in Herefordshire.

On Saturday 29 December 2012, at 10.30 pm GMT, the British Geological Survey recorded a Magnitude 1.4 Earthquake at a depth of 14 km beneath southwest Herefordshire, roughly 15 km southwest of Hereford and 20 km west of Ross-on-Wye. This is far too small and too deep to have caused any damage or injuries, and may not have been felt at the surface at all.

The location of the 29 December 2012 Earthquake. Google Maps.

There is no overridingly obvious cause for most Earthquakes in the UK; the country is subject to tectonic pressures from a number of sources, and most quakes are thought to be a combination of more than one of these. Britain is being pushed to the east by the expansion of the Atlantic Ocean (along with the rest of Eurasia) and to the north by the impact of the African Plate into Europe from the south. There are also lesser areas of geological expansion beneath the North Sea, the Rhine Valley and the Bay of Biscay, all of which exert some pressure on UK rocks. Finally there is glacial rebound; until about 10 000 years ago much of the north of the UK was covered by a thick layer of glacial ice, which pushed the rocks of the British lithosphere down into the underlying mantle. This ice is now gone, and the rocks are slowly springing back into place, causing the occasional Earthquake in the process, though this is more of an issue further to the north, particularly on the west coast of Scotland, the most quake-prone part of the country.

Witness reports can be important in helping geologists to understand the processes going on in Earthquakes. If you felt this quake (or were in the area but didn't, which is also useful information) you can report it to the British Geological Survey here.


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Saturday, 22 December 2012

A Jurassic Turtle bone-bed from the far northwest of China.

Turtles are aquatic reptiles with a shell that encases their body, and into which the head and limbs can be retracted at least partially. They have a fossil record that dates back to the Late Triassic, about 220 million years ago, and they have been an important part of many marine and freshwater ecosystems ever since. Their exact relationship to other reptiles is difficult to determine from morphological evidence since their bodies have become so heavily modified, but genetic studies suggest that they are a sister group to the Archosaurs (Crocodiles, Dinosaurs and Birds).

In a paper published in the journal Naturwissenschaften on 21 October 2012, a team of scientists led by Oliver Wings of the Museum für Naturkunde in Berlin and the Department of Geosciences at Universität Tübingen, describe an extraordinary fossil bone-bed from the Turpan Basin of northern Xinjiang Province in the far northwest of China.

The location of the Turtle bone bed (above) and a photograph of the outcrop (bellow). Wings et al. (2012).

The outcrop is referred to by Wings et al. as 'Messa Chelonia'; it is roughly 25 km east of the city of Shanshan. Fossil turtles were exposed along a 30 m wide outcrop, located by the Sino-German Cooperation Project in 2008. A half meter square block was removed in 2009 and prepared in Shanshan; several more blocks were removed in 2011, but have not yet been worked on.

The deposit is believed to be late Middle Jurassic in age, making it about 165 million years old. All the Turtles present appear to belong to a single species, Annemys sp.. Wings et al. suggest that they died in a mass mortality event around pools in a drying river-bed during a prolonged drought, then were concentrated by a flash flood when the draught broke. 

(a) The material recovered from the Mesa Chelonia site in 2009, and partially prepared within its plaster and burlap case. (b) Schematic drawing of the Turtles within the block; some Turtles are shown which have been removed in the photograph. Wings et al. (2012).

Annemys sp. from the late Middle Jurassic Konzentratlagerstätte at Mesa Chelonia, Xinjiang Autonomous Province, China: (a) carapace and (b) plastron; (c) carapace (d) carapace and (e) plastron; (f) dorsal view and (g) ventral view of skull; (h) position of depicted fossils within the block recovered from the fossil rich inner zone of the Konzentratlagerstätte. Abbreviations: Abd abdominal scute, An anal scute, bo basioccipital, bps basisphenoid, co costal, epi epiplastron, ex exoccipital, Fe femoral scute, fpccc foramen posterius canalis caroticum cerebrale, fpcci foramen posterius canalis caroticum interni, fpccl foramen posterius canalis caroticum laterale, fpp foramen palatinum posterius, fr frontal, Hu humeral scute, hyo hyoplastron, hypo hypoplastron, ju jugal, Ma marginal scute, mx maxilla, na nasal, ne neural, nu nuchal, op opisthotic, pa parietal, pal palatine, Pec pectoral scute, per peripheral, pf prefrontal, Pl pleural scute, pmx premaxilla, po postorbital, pro prootic, pt pterygoid, qu quadrate, so supraoccipital, sq squamosal, V vertebral scute, vo vomer, xi xiphiplastron. Wings et al. (2012).


Wings et al. estimate that the bone bed covers an area of at least 20 m², and contains at least 720 Turtles, and may be as large as 236 m², with as many as 1800 Turtles.


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Wednesday, 19 December 2012

Goblin Spiders from Cretaceous Amber.

Goblin Spiders (Oonopidae) are one of the most abundant groups of Spiders, with at least 600 and possibly over 1000 extant species described, though this is generally considered to be a poor representation of their diversity, since the Spiders are tiny (often under 1 mm) and at their most abundant in the tropics. Goblin Spiders have a fossil record that dates back to the Cretaceous, being quite common in amber, though not known from sedimentary rocks. Goblin Spiders have six eyes rather than the eight of most Spiders, though some species have lost additional eyes. The back pair of legs are modified for jumping.

In a paper published in the journal Palaeontology in January 2012, a team of scientists led by Erin Saupe of the Department of Geology & Paleontological Institute at the University of Kansas describe four new Goblin Spider specimens from Cretaceous Amber from France and Spain. All the Spiders are placed in the genus Orchestina, which is still extant. Only two specimens are assigned to species, the other two (probably) being females, which are hard to distinguish to species level in modern specimens.

The first new Spider described is named Orchestina gappi, after Ian Wesley Gapp, a student at the University of Kansas. Orchestina gappi is a 1 mm Goblin spider preserved in a piece of dark brown, opaque amber from the Font-de-Benon Quarry, 1 km east of Archingeay-Les Nouillers in the Charente-Maritime Department of France. The sediments from which the amber was recovered are uppermost Albian–lowermost Cenomanian in age, making the fossil roughly 100 million years old. The specimen is barely visible through the dark amber matrix, but was revealed by synchrotron imaging at the European Synchrotron Radiation Facility in Grenoble.

Synchrotron images of Orchestina gappi. Scale bar is 1 mm. Saupe et al. (2012).

The second specimen is named Orchestina rabagensis, after the Rábago, the municipality in Cantabria, Spain where the fossil was found. Orchestina rabagensis is a 1.1 mm Goblin Spider preserved in light
yellow amber from the El Soplao Outcrop. It is early Albian in age, or about 110-113 million years old.

Orchestina ragagensis: (Top) Photograph and (Bottom) interpretive drawing. Stars indicate the locations of trichobothria, sensitive hairs capable of detecting air movements. Scale bars are 0.5 mm. Saupe et al. (2012).

The first unnamed specimen is a 1.11 mm female(?) Goblin Spider preserved in clear orange amber from the San Just Outcrop at Teruel in Spain. It is Middle Albian in age, or about 105 million years old.

Orchestina sp. from the San Just Outcrop. (Top) Photograph, scale bar is 0.5 mm. (Bottom) Synchrotron images, scale bar is 1 mm. Saupe et al. (2012).

The second unnamed specimen is a female over 1 mm in length from embedded in a piece of clear, dark orange amber, slightly clouded by organic debris. The specimen was found at the Peñacerrada Outcrop in Burgos, Spain. It is early Albian in age, or about 110-113 million years old.

Orchestina sp. from the Peñacerrada Outcrop. (Top) photograph, (Bottom) interpretive drawing. Stars indicate known trichobothria. C = crack, B = bubble. Scale bars represent 0.5 mm. Saupe et al. (2012).


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Tuesday, 27 November 2012

Soft tissue preservation in Linguloid Brachiopods from the Early Ordovician Fenxiang Formation of Hubei Province, China.

Brachiopods (or Lampshells) superficially resemble Bivalve Molluscs, though they are not closely related. They have a filter feeding apparatus called a lophophore, unlike anything found in any Mollusc, but also found in Bryozoans and Phoronid Worms. This is encased with in a shell with two valves, each symmetrical about a midline, but not necessarily the same as each other, along with the rest of the organs of the body; there is typically remarkably little flesh to a Brachiopod compared to a Mollusc with a shell the same size. However one group of Brachiopods, the Linguloids, which have a long, fleshy, worm-like body with a shell enclosing only the head-area; these Brachiopods have been compared to a Phoronid Worm with a partial shell, and are considered to be the earliest group of Brachiopods; they appear in the fossil record early in the Cambrian, and essentially unchanged forms still exist today.


Modern Linguloid Brachiopods. Suny Cortland.

In a paper published in the journal Acta Palaeontologica Polonica on 1 October 2012, Andrzej Baliński of the Instytut Paleobiologii at the Polish Academy of Sciences and Yuanlin Sun of the Key Laboratory of Orogenic Belts and Crustal Evolution at the School of Earth and Space Sciences at Peking University describe the occurrence of Linguloid Brachiopods with preserved soft-tissue tails from the early Ordovician Fenxiang Formation of Hubei Province, China.

This is not the oldest such occurrence, Linguloid Brachiopods have been found with their tails preserved in both the Burgess Shale and Chengjang Faunas from the Cambrian, but it is still a significant find. The Cambrian specimens are not universally accepted as having been burrowing animals; some scientists believe that in the rather different ecosystems of the Early Cambrian they may not have needed to burrow; there is certainly no clear evidence of burrowing by any form of animal from sediments of this time. The Ordovician is a different matter, burrowing lifestyles had definitely evolved by this time, and there was no shortage of predators available to attack an exposed Linguloid Brachiopod on the surface.

The method of preservation is also different to that seen in the Cambrian fossils, which are preserved as two-dimensional aluminosilicate or degraded organic carbon films in shales (laminated mudstones), a method of preservation extremely rare after the Early Cambrian due to bioturbation of marine sediments by burrowing animals. In contrast these Ordovician fossils are preserved as three-dimensional mineralized body-fossils. In these specimens the mineralized soft tissue is a bright-red colour, due to the oxidation of iron minerals. The soft tissues are thought to have initially been replaced with hydrogen sulphide (H₂S) by sulphur-reducing bacteria in an anaerobic (oxygen-lacking environment), this Hydrogen Sulphide is then thought to have reacted with iron from the surrounding sediments, giving it its distinctive colour.

Preserved Linguloid Brachiopod from the lower Ordovician Fenxiang Formation. Scale bar is 5 mm. Baliński & Sun (2012).


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