How subtle are the biases that shape the fidelity of the fossil record? A test using marine molluscs

Biases in preservation shape the fossil record, and therefore impact on our reconstructions of past environments and biodiversity. Given the intensive recent research in the general fields of taphonomy and exceptional preservation, surprisingly, fundamental questions remain unanswered about species-level variation in skeletal preservation potential at low taxonomic levels (e.g. between genera from the same family, or between taxa from related families) across myriad groups with multi-element skeletons. Polyplacophoran molluscs (chitons sensu lato) are known from the late Cambrian to Recent, and possess a distinctive articulated scleritome consisting of eight overlapping calcareous valves. The apparent uniformity of living chitons presents an ideal model to test the potential for taphonomic biases at the alpha-taxon level. The vast majority of fossil chitons are preserved as single valves; few exhibit body preservation or even an articulated shell series. An experimental taphonomic programme was conducted using the Recent polyplacophorans Lepidochitona cinerea and Tonicella marmorea (suborder Chitonina) and Acanthochitona crinita (Acanthochitonina). Experiments in a rock tumbler on disarticulated valves found differential resistance to abrasion between taxa; in one experiment 53.8-61.5% of Lepidochitona valves were recovered but 92% of those from Tonicella and 100% of elements from Acanthochitona. Chiton valves and even partly decayed carcasses are more resistant to transportation than their limited fossil record implies. Different species of living chitons have distinctly different preservation potential. This, problematically, does not correlate with obvious differences in gross valve morphology; some, but not all, of the differences correlate with phylogeny. Decay alone is sufficient to exacerbate differences in preservation potential of multi-element skeletons; some, but not all, of the variation that results is due to specimen size and the fidelity of the fossil record will thus vary intra-specifically (e.g. between ontogenetic stages) as well as inter-specifically. 

Reading Maud’s remains: Tennyson, geological processes, and palaeontological reconstructions

As Tennyson's “little Hamlet ,” Maud (1855) posits a speaker who, like Hamlet, confronts the ignominious fate of dead remains. Maud's speaker contemplates such remains as bone, hair, shell, and he experiences his world as one composed of hard inorganic matter, such things as rocks, gems, flint, stone, coal, and gold. While Maud's imagery of “stones, and hard substances” has been read as signifying the speaker's desire “unnaturally to harden himself into insensibility” (Killham 231, 235), I argue that these substances benefit from being read in the context of Tennyson's wider understanding of geological processes. Along with highlighting these materials, the text's imagery focuses on processes of fossilisation, while Maud's characters appear to be in the grip of an insidious petrification. Despite the preoccupation with geological materials and processes, the poem has received little critical attention in these terms. Dennis R. Dean, for example, whose Tennyson and Geology (1985) is still the most rigorous study of the sources of Tennyson's knowledge of geology, does not detect a geological register in the poem, arguing that by the time Tennyson began to write Maud, he was “relatively at ease with the geological world” (Dean 21). I argue, however, that Maud reveals that Tennyson was anything but “at ease” with geology. While In Memoriam (1851) wrestles with religious doubt that is both initiated, and, to some extent, alleviated by geological theories, it finally affirms the transcendence of spirit over matter. Maud, conversely, gravitates towards the ground, concerning itself with the corporal remains of life and with the agents of change that operate on all matter. Influenced by his reading of geology, and particularly Charles Lyell's provocative writings on the embedding and fossilisation of organic material in strata in his Principles of Geology (1830–33) volume 2, Tennyson's poem probes the taphonomic processes that result in the incorporation of dead remains and even living flesh into the geological system.

Dificultades en el uso de las preposiciones en estudiantes francófonos de ELE

Ce projet de maîtrise se consacre à l’apprentissage des prépositions espagnoles chez les élèves francophones. L’identification et l’analyse des erreurs les plus fréquentes dans l’usage des prépositions par des francophones nous permettrons d’élaborer des exercices pratiques qui rendraient leur apprentissage moins difficile. Nous croyons que la difficulté dans l’utilisation des prépositions chez les étudiants réside en partie dans le fait de ne pas connaître leur emploi exact. Nous commencerons donc par présenter l’emploi des principales prépositions en espagnol à partir du Manual de la Nueva gramática de la lengua española et d’autres études. L’enseignement de la grammaire dans les cours d’espagnol comme langue étrangère (ELE) au Québec suit les règles établies par le Cadre européen commun et le Plan curricular de l’Institut Cervantès. Les étudiants développent leur compétence grammaticale de manière inductive; ils sont amenés à comprendre les règles par eux-mêmes et à créer leurs propres hypothèses qu’ils confirment ou réfutent après grâce à quelques explications formelles de l’enseignant et des exercices de pratique. Par contre, cette tendance à laisser l’apprentissage de la grammaire entre les mains des étudiants peut aussi amener à la fossilisation de leurs erreurs si les explications et la pratique ne sont pas suffisantes. Les erreurs sont perçues comme un point de départ pour comprendre où résident les difficultés des étudiants et permettent aux enseignants d’apporter les changements nécessaires à leurs méthodes d’enseignement. Notre révision de quelques investigations réalisées avec la méthode de l’analyse des erreurs, nous permet de cerner les raisons pour lesquelles les francophones commettent autant d’erreurs dans l’utilisation des prépositions espagnoles. Notre analyse de l’enseignement et de la pratique des prépositions dans trois manuels qui s’utilisent actuellement dans les cégeps et les universités du Québec nous permet de voir que les prépositions ne se pratiquent pas assez, surtout au niveau intermédiaire. Nous proposons donc des exercices pratiques qui permettront aux étudiants de pratiquer les prépositions de manière plus efficace.

On wing disparity and morphological variation of the Santana Group pterosaurs

Pterosaurs were widely spread throughout the Mesozoic Era, populating the whole world. Among this great diversity, two groups are commonly found in Brazil: the Anhangueridae and Tapejaridae. These can be mainly identified by cranial synapomorphies. However, because of the fragility of the pterosaur skeleton and rarity of the fossilisation process, the fossils found are usually incomplete, which hampers a proper taxonomic identification of the specimens. The specific proportions of these two groups of pterosaurs were obtained from bibliographic data and measurements of specimens. Eight Anhangueridae-like and seven Tapejaridae were used: Anhanguera piscator, Anhanguera santanae, Anhanguera spielbergi, Araripesaurus castilhoi, Barbosania gracilisrostris and three Anhangueridae sp. indet.; Sinopterus dongi, Tapejara wellnhoferi and five Tapejaridae sp. indet. We find that proportions of the humerus, wing metacarpal, first phalanx of the wing digit, femur and tibia are sufficient to identify partial remains of Araripe pterosaurs. A principal component analysis shows that each clade has different, non-overlapping scores in the studied ratios and these can be used with precision. Specific bone ratios for fast identification of anhanguerids and tapejarids are given, opening a broader way to diagnostic fragmentary bones.