Trace fossils formed by heart urchins - a study of Scolicia and related traces

Cretaceous and Tertiary traces belonging to the ichnogenera Scolicia, Subphyllochorda and Taphrhelminthopsis are described and analysed functionally. Resting traces continuous with Subphyllochorda are described for the first time and interpreted as the work of heart urchins. The new ichnogenus Cardioichnus is erected for them. The preservation and complexity of some specimens of these ichnogenera allows for a detailed comparison with heart urchin morphology. Subphyllochorda is interpreted as a burrow produced by heart urchins and Scolicia as either burrows or sea floor furrows. The traces here assigned to Taphrhelminthopsis are probably casts of washed-out Subphyllochorda burrows. Palaeozoic traces previously referred to 'Scolicia' sensu lato are, in the main, much simpler than the Mesozoic and Tertiary traces and should be transferred to other ichnogenera.     

Modern and fossil traces in terrestrial lithic substrates

A number of biogenic processes leads to the formation of distinctive traces in terrestrial lithic substrates. These include: burrowing by vertebrates in moderately lithified rocks; scraping by mammals; smoothing and polishing of limestone surfaces by the locomotion of mammals; excavation by bees, wasps, and ants producing nesting and dwelling tunnels; dissolution of limestone surfaces by terrestrial snails; endolithic activity of fungi, algae, and lichens on subaerial rock surfaces; root corrosion; etc. Processes of biochemical weathering, biophysical erosion, and enlargement of cracks and fissures by the pressure of plant roots do not leave distinctive traces and therefore lie outside the ichnological realm. The fossil preservation of terrestrial bioerosional traces is expected to be uncommon. Nevertheless, various possible means of preservation must be considered, such as by rapid burial by volcanic material, by fluvial sediments, by travertine or tufa, by loess, “conservation”; in caves, case hardening of surfaces of porous rocks, and preservation of subsoil traces below fossil soils.     

The retroactive action of paradoxical sleep deprivation and immobilization stress on the mechanisms of memory and passive avoidance in rats

Influence was studied of 48-hours deprivation of paradoxical sleep (DPS) and immobilization stress on conditioned reaction of fear and security--components of passive avoidance conditioned reflex (CRPA), with simultaneous studying of vertical, horizontal activity, grooming reactions and defecations in an illuminated chamber. The obtained results allow to conclude that DPS inhibits reproduction of memory traces of fear reaction but intensifies the process of learning and activity of memory traces of security reaction. Depending on condition of CRPA elaboration, DPS may disturb or, on the contrary, prolong preservation of passive avoidance. It has been found that the immobilization stress does not influence CRPA preservation and does not weaken the reaction of fear but increases the horizontal activity. It is suggested that the observed changes in behaviour and trace processes are connected with disturbance of sensory informational homeostasis of the nervous system at DPS.     

Traces of a possible Celtic brewery in Eberdingen-Hochdorf, Kreis Ludwigsburg, southwest Germany

A large number of weakly germinated hulled barley grains was found during archaeobotanical analyses from the early Celtic settlement excavations at Eberdingen-Hochdorf in southwest Germany (ca. 600 – 400 BC). These grains seem to represent deliberate germination, due to the purity of the find and its unusual archaeological context. The possibility of deliberate malting which could be connected with beer brewing is discussed. Recent germination and charring experiments show that the consistently weak traces of germination on the charred subfossil grains from Hochdorf are enough to indicate malted grains. A comparison of the archaeobotanical remains with the written and archaeological sources shows that evidence of beer brewing from excavations is very scarce. There is practically no clear proof of brewing, while written sources and indirect suggestions are abundant. Neither archaeological finds nor either written or iconographic sources give exact details about the prehistoric brewing technology of the early Celts. The archaeological finds from Hochdorf seem to be the result of deliberate malting of hulled barley for the purpose of Celtic beer brewing.     

Effects of timber harvest on phlebotomine sand flies (Diptera: Psychodidae) in a production forest: abundance of species on tree trunks and prevalence of trypanosomatids

The Amazon forest is being exploited for timber production. The harvest removes trees, used by sand flies as resting sites, and decreases the canopy, used as refuges by some hosts. The present study evaluated the impact of the timber harvest, the abundance of sand flies, and their trypanosomatid infection rates before and after selective logging. The study was accomplished in terra-firme production forest in an area of timber harvest, state of Amazonas, Brazil. Sand fly catches were carried out in three areas: one before and after the timber harvest, and two control areas, a nature preservation area and a previously exploited area. The flies were caught by aspiration on tree trunks. Samples of sand flies were dissected for parasitological examination. In the site that suffered a harvest, a larger number of individuals was caught before the selective extraction of timber, showing significant difference in relation to the number of individuals and their flagellate infection rates after the logging. The other two areas did not show differences among their sand fly populations. This fact is suggestive of a fauna sensitive to the environmental alterations associated with selective logging.     

A Curious Rusophycus (Arthropod Ichnofossil) Assemblage from the Upper Ordovician of Ontario,Canada

The ichnogenus Rusophycus includes a wide range of short bilobate excavations generally attributed to variable feeding behaviors of arthropods, especially trilobites. An unusual Rusophycus assemblage from Upper Ordovician Georgian Bay Formation in Ontario departs radically from previously described examples and presents new challenges for understanding the behavior represented by these traces. This specimen is unique in the arrangement of multiple Rusophycus burrows in a circular, lens-shaped array (as opposed to a linear or random arrangement typical of other Rusophycus assemblages). The size and shape of the individual Rusophycus components are consistent with traces attributed to the coeval trilobite Flexicalymene. Multiple Rusophycus assemblages likely reflect aggregations of trilobites in response to a local concentration of food. The topology of this particular Rusophycus assemblage suggests that the trilobites opportunistically exploited a rich and narrowly restricted food source, perhaps the decaying remains of a buried organism.     

Bone and ivory points in the Lower and Middle Paleolithic of Europe.

The existence of shaped bone and ivory points, to be used as awls or with wooden hafts, has been suggested for the Lower Paleolithic sites of Torralba and Ambrona and for several Middle Paleolithic sites, such as Vaufrey, Combe Grenal, Pech de l'Azé I and Camiac. The use of hafted bone and ivory points would imply a spear armature technology similar to that well documented in the Upper Paleolithic, often considered an innovation introduced to Europe by anatomically modern humans.The controversial ivory points from the two Spanish sites, whose fracture morphology is considered natural by G. Haynes (1991), have been reanalyzed, checking for putative traces of human manufacture and utilization as described by Howell & Freeman (1983), i.e., polish, flaking of stem, ground edges, striations from manufacture and contact with a haft or binding. We have been able to study 19 new proboscidean tusk tips from the ongoing Ambrona excavations by a Spanish team. For these and nine other Middle Paleolithic bone and antler points we use optical and SEM microscope analysis, taphonomic analysis, comparative observations of Upper Paleolithic bone points, experimental observations of manufacturing traces, modern tusk samples, and data on several bone and antler pseudo-points from carnivore accumulations.We show that none of the objects we have studied can be interpreted as an intentionally shaped point. The absence of hafted bone points in the Middle Paleolithic of Europe is contrasted with evidence of the use of hafted stone points since OIS 5 or earlier in Eurasia and Africa. We suggest that the absence of organic spear armatures in the Middle Paleolithic is not due to a deficiency in the technology of Neandertals but may be tied to the organizational strategies of the hunters and to patterns of game choice and capture.     

克隆整合对无芒雀麦(Bromus inermis)忍受沙埋能力的影响

无芒雀麦是浑善达克沙地植物群落中占优势的多年生根茎禾草。研究了克隆整合特性对无芒雀麦忍受沙埋能力的影响。结果表明,克隆整合显著提高了远端完全沙埋分株的存活,耗-益分析表明远端沙埋分株的生物量、分株数、叶片数、根茎节数和根茎总长显著受益于克隆整合,而与之相连的近端非沙埋分株却没有产生显著的损耗,并且随着沙埋程度增加时,远端沙埋分株的收益有增大的趋势。因而,克隆整合特性是无芒雀麦对严酷沙埋环境形成的重要适应对策,它能够缓解沙埋对无芒雀麦存活、生长的胁迫,提高其在半干旱沙化地区的适合度。     

New Insights into Polychaete Traces and Fecal Pellets: Another Complex Ichnotaxon?

Neoichnological observations help refine paleoichnological records. The present study reports extensive observations on the distribution, morphology, occurrence and association of burrows and fecal pellets of the polychaete Nereis diversicolor in the Kundalika Estuary on the west coast of India. Our holistic study of these modern-day traces suggests it to be a complex trace arising from domichnial, fodinichnial and possibly pascichnial behavior of polychaetes. The study for the first time reports extensive fecal pellet production, distribution and their preservation as thick stacks in modern estuarine environment. These observations testify the fossilization potential of pellets and provide an explanation to their origin in the geological record. Their occurrence as strings associated with mounds not only suggests pascichnial behaviour of polychaetes but also allows the assignment of post-Paleozoic Tomaculum to the activity of polychaete worms. The production of fecal pellets in such large quantities plays a major role in increasing the average grain size of the substrate of these estuarine tidal flats, thereby improving aeration within the substrate.     

Morphological preservation of carbonaceous plant fossils in blueschist metamorphic rocks from New Zealand

Morphological and chemical evidence of ancient life is widespread in sedimentary rocks retrieved from shallow depths in the Earth's crust. Metamorphism is highly detrimental to the preservation of biological information in rocks, thus limiting the geological record in which traces of life might be found. Deformation and increasing pressure/temperature during deep burial may alter the morphology as well as the composition and structure of both the organic and mineral constituents of fossils. However, microspore fossils have been previously observed in intensely metamorphosed rocks. It has been suggested that their small size, and/or the nature of the polymer composing their wall, and/or the mineralogy of their surrounding matrix were key parameters explaining their exceptional preservation. Here, we describe the remarkable morphological preservation of plant macrofossils in blueschist metamorphic rocks from New Zealand containing lawsonite. Leaves and stems can be easily identified at the macroscale. At the microscale, polygonal structures with walls mineralized by micas within the leaf midribs and blades may derive from the original cellular ultrastructure or, alternatively, from the shrinkage during burial of the gelified remnants of the leaves in an abiotic process. Processes and important parameters involved in the remarkable preservation of these fossils during metamorphism are discussed. Despite the excellent morphological preservation, the initial biological polymers have been completely transformed to graphitic carbonaceous matter down to the nanometer scale. This occurrence demonstrates that plant macrofossils may experience major geodynamic processes such as metamorphism and exhumation involving deep changes and homogenization of their carbon chemistry and structure but still retain their morphology with remarkable integrity even if they are not shielded by any hard-mineralized concretion.     

Preferential predatory peeling: Ammonoid vs. nautiloid shells from the Upper Carboniferous of Texas,USA

Narrow groove-like excavations on ammonoid and coiled nautiloid shells are rare in Upper Carboniferous units from Texas, USA. The morphological characteristics of the excavation grooves typically are confined to the ventral and ventrolateral parts of the outer whorl of the shell, are narrower than the length, and have irregular edges where small segments or chips of shells have been removed. Analysis of these features reveals a statistically significant preferential occurrence on ammonoids (1.195% of ca. 3515 specimens) as compared to coiled nautiloids (0.506% of ca. 2965 specimens). The ammonoids typically have longer excavations that penetrate the phragmocone more frequently than those observed in the coiled nautiloids. The groove-like excavations were probably formed by the removal and peeling of shell material by one or more predatory or scavenging arthropods to obtain organic material (tissue and membranes) within the ammonoid and nautiloid body chambers and phragmocones. The excavations probably occurred when the cephalopod was alive (i.e., the cause of death) or shortly after the cephalopod's death. There is no evidence that the excavations are related to sheltering by the excavating organism.     

Borings in mobile clasts from Eocene conglomerates of Northern Dalmatia (Coastal Dinarides, Croatia)

Summary Bored clasts occur in Eocene conglomerates deposited in the upper shoreface and beachface settings of the Dinaric foreland basin. The trace fossil assemblage consists ofGastrochaenolites, Trypanites, and possibly some other ichnotaxa and may be compared to theTrypanites Ichnofacies. The preservation characteristics of the borings reflect many stages of colonisation/boring and abrasion. The removal of shells of the boring bivalves, the different depths of the abrasional truncation of borings, and the predominant preservation of the largest excavations (Gastrochaenolites) in the ichnocoenosis are related to repeated phases of abrasion, caused by the mobility of clasts. Coastal gravel is a specific variant of hard substrates, whose mobility controls the colonisation of borers, the type of assemblage and its preservation potential.     

Asteroid and Ophiuroid Trace Fossils from the Lower Cretaceous of Chile

Abundant asterozoan trace fossils in the Lower Cretaceous Apeleg Formation of southern Chile were produced by the infilling of traces made by asteroids and ophiuroids on a muddy surface. Most are preserved as hypichnial ridges formed as casts on the bottom of fine-grained sandstone laminae. Star-shaped Asteriacites lumbricalis are interpreted as the infillings of shallow excavations made by asteroids. Hook-shaped and sinuous ridges of the newly defined ichnogenus and ichnospecies Ophioichnus aysenensis are interpreted as the casts of imprints made by the walking action of the arms of ophiuroids. Deposition probably took place in an offshore tide-swept marine shelf environment. In life the animals formed an assemblage equivalent to echinoderm aggregations on the modern sea floor.     

Synthèse sur la diversité des préservations végétales du site d’Archingeay-Les Nouillers (France) : un Konservat-Lagerstätte pour les flores de l’Albien-Cénomanien

Since the end of the XXth century, the palaeontological site of Archingeay-Les Nouillers (Charente-Maritime, western France) continued to afford Albian-Cenomanian (ca 93–113 Ma) plant meso- and macroremains. The successive excavations provided numerous specimens useful for the reconstruction of mid-Cretaceous coastal forest ecosystems. However, one of the most remarkable features of this locality is the diversity of plant preservations. Unique in Europe from this point of view, the fossiliferous site of Archingeay-Les Nouillers yielded compressions with or without cuticle, impressions/imprints, and silicified permineralizations/petrifications. The quality of the silicified tissues and the cell preservation allow this locality to be considered as a plant Konservat-Lagerstätte.     

The Oldowan site Aïn al Fil (El Kowm,Syria) and the first humans of the Syrian Desert

At present, the oldest traces of human cultures are found in Eastern Africa. New discoveries set anew the questions about human and animal dispersal into Eurasia. For over 1.8 million years, humans have been present in the Levant. An extensive program of surveys and excavations in the Syrian Desert showed that this part of the world was a very ancient land of settlement. In Central Syria, the oldest site, Aïn al Fil in the region of El Kowm, was excavated in 2008 and 2010. The lithic industry in the lowest layer can be characterized by numerous unretouched flakes, pebble-tools and core-like artefacts. This assemblage is typical in a broad sense of archaic Palaeolithic the debitage of which corresponds to mode 1. From a techno-typological point of view, this industry tallies quite well with the so-called Oldowan stage. It shows remarkable similarities with the oldest African assemblages. From a chronologic point of view, these levels occur before three positive events in the Matuyama paleomagnetic sequence. It seems consistent to place the Oldowan sequence around 1.8 Ma BP within the Olduvai subchron or just before Olduvai/Matuyama reversal limit. Together with those of the neighbouring site Hummal, these levels would be the oldest traces of human presence ever found in Syria. In the Levant, the first humans not only occupied favourable zones but regularly ventured deep into less welcoming environments suggesting an astonishing flexibility in their behavioural and survival skills.     

Paleolimulus, an early limuline (Xiphosurida), from Pennsylvanian-Permian Lagerst tten of Kansas and taphonomic comparison with modern Limulus

The Pennsylvanian-Permian horseshoe crab Paleolimulus signatus (Beecher), incorporating as a junior synonym P. avitus Dunbar, is one of the earliest species of the Limulina (Xiphosurida). Some specimens from Kansas, USA, are exceptionally well preserved, retaining intact book gills and appendages. Indistinct, bilobed burrowing traces of variable width occur in association with some examples of P. signatus and may have been produced by that animal. Based on actualistic taphonomic experiments on Limulus polyphemus, ancient horseshoe crabs and other arthropods having non-mineralized exoskeletons are inferred to have become pliable soon after death or moulting, and to have disarticulated slowly prior to burial. Extreme compression, wrinkling, and loose folding of sclerites are attributed to burial of a pliable exoskeleton. Slow preburial disarticulation partly accounts for the exceptional preservation of Paleolimulus remains. Also relevant for the exceptional preservation of these arthropods was burial in estuarine, tidal flat, or lacustrine environments. Because of fluctuating salinity and possibly dessicating conditions, these settings were limiting to scavengers, burrowers, and some microbes that could potentially disarticulate or decompose xiphosurid remains.     

Dual-color bioluminescent assay using infected HepG2 cells sheds new light on Chlamydia pneumoniae and human cytomegalovirus effects on human cholesterol 7α-hydroxylase (CYP7A1) transcription

Human bones, recovered from excavations, are an important biological archive of information. In particular, the analysis of the collagen fraction is useful for paleodietary reconstruction, via light stable isotopes, and for (14)C dating. Generally, collagen extraction procedures do not prevent loss of integrity of proteins. As a consequence, information about the state-of-remains preservation is unavailable. Here we describe a "soft" nondestructive CH(3)COOH-based method to recover collagen from archaeological bones, and also to obtain material for successive isotopic analyses. Our isotopic measurements on the extracts indicate that the CH(3)COOH-based method of extraction may be routinely employed in the context of paleodiet studies. In addition, we propose that biochemical characterization by denaturant electrophoresis and Western blot on CH(3)COOH extracts may be used as a bone collagen quality indicator.     

Remarkably preserved benthic organisms and their traces from a Middle Triassic (Muschelkalk) mud flat

Knaust, D. 2010: Remarkably preserved benthic organisms and their traces from a Middle Triassic (Muschelkalk) mud flat. Lethaia, Vol. 43, pp. 344–356. A new Fossil‐Lagerstätte is reported from the Middle Triassic of Germany, preserving Foraminifera, Nematoda, Platyhelminthes, Nemertea, Annelida and a range of Arthropoda together with their traces. This is the oldest fossil record of free‐living nematodes and turbellarians, and the first occurrence of nemerteans in the Mesozoic. The rare preservation of the benthic associations together with their traces is unique; especially the abundant occurrence of different phyla as meiofauna (organisms with shortest dimension between 0.06 and 1 mm) provides an insight into the palaeoecological conditions of a 240‐Ma‐old muddy tidal flat. The preservation of benthic animals at the termination of their traces offers the exclusive opportunity to assign producers to the trace fossils. The results show that the discussed phyla were already established in the early Mesozoic in a similar diversity and composition as in modern analogues. The new Fossil‐Lagerstätte has the potential to prove a number of soft‐bodied taxa immediately after the end‐Permian mass extinction, which has wide‐ranging implications for phylogenetic interpretations. □Benthos, soft‐bodied organisms, Fossil‐Lagerstätte, Muschelkalk, trace fossils, Triassic.     

Herbivory by subterranean termite colonies and the development of fairy circles in SW Namibia

1. The growth pattern of Namibian fairy circles was examined in relation to environmental, termite, and plant variables to provide support for the sand termite (Psammotermes allocerus Silvestri) hypothesis of circle origin. 2. New and young circles were associated with the highest number of sand termites and their foraging grass sheetings which were both considerably lower in mature and senescent circles. 3. Circles increased in size with age, and apart from the senescent stage had higher soil moisture levels than the matrix. 4. In laboratory trials sand termites browsed seedling roots, negatively impacting root and leaf number. 5. This provides a potential mechanism for circle formation through central‐based foraging by P. allocerus which eliminates Stipagrostis grass clumps around its nest system. 6. The resulting bare disc is postulated to be maintained through a combination of a depleted seed bank, termite herbivory on seedlings, and excavations by pugnacious ants (Anoplolepis steingroeveri Forel).