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Daley, A. C.

Publications and source records attributed to Daley, A. C..

5 recordsLinked to original sources

Morphological characterization of moulting in the Atlantic horseshoecrab Limulus polyphemus: phylogenetic conservation amongchelicerates and evolutionary convergence of ecdysis linked to headshield patterns

Arthropods must periodically moult their exoskeleton to permit growth, a conserved developmental process whose morphological and behavioural execution varies widely among lineages. Horseshoe crabs (Limulidae) are members of Xiphosura, a chelicerate lineage with a fossil record extending as far back as the Ordovician and provide a valuable comparative framework for studying the evolution of moulting strategies in Arthropoda. Despite their importance, detailed morphological characterization of moulting in horseshoe crabs remains scarce, limiting developmental studies and broader comparative analyses. Here, we provide a detailed morphological characterization of the moulting process in the Atlantic horseshoe crab Limulus polyphemus. Morphological changes in specific anatomical structures, including the anterior margin of the prosoma, lateral spines and dorsal spinous process of the opisthosoma, were observed during the moulting process. By tracking these morphological markers, such as retraction of the epidermis from the cuticle and degree of corrugation of the epidermis, we were able to identify individuals in the early and late pre-moult stage, predict the onset of ecdysis, and distinguish post-moult and intermoult stages. We compare ecdysis patterns in L. polyphemus with other arthropod taxa, both extant and fossil. We find that, despite differences in behavioural execution, ecdysis in L. polyphemus shares features with other chelicerates, and that both phylogenetic signal and convergent patterns are evident across Arthropoda. This study offers a robust, non-invasive method for determining moult stages in juvenile horseshoe crabs and provides insights into the diversity and constraints of ecdysis in Arthropoda.

evolutionary biology↗

Moult cycle and setal development of the Atlantic ditch shrimp Palaemon varians Leach, 1814

The Atlantic ditch shrimp Palaemon varians Leach, 1814 is a common estuarine and brackish water species on Northern Atlantic coasts. Palaemon varians is an appealing model organism for studying arthropod developmental processes, such as moulting (ecdysis). Detailed morphological information on its moult cycle is still lacking, hence we have characterised the changes in the setal features corresponding to the moult stages of P. varians grown under laboratory conditions. The stages of the moult cycle were differentiated and described using microscopic analysis of the setae in the uropods of P. varians based on Drachs classification system. Moult stages were defined as early and late post-moult (A and B), inter-moult (C), early-, mid- and late pre-moult (D0, D1, and D2), as well as ecdysis stage (E), the actual shedding of the exuvia. Average moult cycle duration was 8.7 days, where pre-moult accounted for the longest duration of 4.4 days on average. This study provides a morphological reference for determining the moult stage of P. varians without the use of invasive techniques, and thus it is well suited for repetitive observations of an individual to track the entire moulting process.

developmental biology↗

New specimens of Bunaia woodwardi, Clarke 1919 (Euchelicerata): A new member of Offacolidae providing insight supporting the Arachnomorpha

The rapid early diversification of arthropods has made understanding internal relationships within the group fiendish. Particularly unresolved is the origin of Euchelicerata, a clade consisting of the Prosomapoda (comprising the extant Xiphosura and Arachnida and the extinct Chasmataspidida, Eurypterida and synziphosurines) and the extinct Offacolidae. Here we describe new material of the Silurian synziphosurine Bunaia woodwardi that reveals previously unknown features of its ventral anatomy: a pair of elongated chelicerae in the prosoma, followed posteriorly by five pairs of biramous appendages, a first pre-abdomen somite bearing a pair of paddle-like uniramous appendages (exopods), and a ventral pretelsonic process. Phylogenetic analyses retrieve B. woodwardi as an Offacolidae closely related to Setapedites abundantis from the early Ordovician Fezouata Biota. An anatomical comparison of the pretelsonic process of B. woodwardi, also present in Setapedites, with the posterior trunk morphologies of other Offacolidae, Habeliida and Vicissicaudata, suggests a possible homologous appendicular origin. This proposed apomorphic character supports a monophyletic Arachnomorpha, formed of Vicissicaudata, Habeliida and Euchelicerata. The establishment of this new homology could help to clarify the highly enigmatic phylogeny at the base of the euchelicerates as well as the sequence of character acquisition during their early evolution.

paleontology↗

The effects of clay minerals on bacterial community composition during arthropod decay

Fossilization, or the transition of an organism from the biosphere to the geosphere, is a complex mechanism involving numerous biological and geological variables. Bacteria are one of the most significant biotic players to decompose organic matter in natural environments, early on during fossilization. However, bacterial processes are difficult to characterize as many different abiotic conditions can influence bacterial efficiency in degrading tissues. One potentially important variable is the composition and nature of the sediment on which a carcass is deposited after death. We experimentally examined this by decaying the marine shrimp Palaemon varians underwater on three different clay sediments. Samples were then analyzed using 16S ribosomal RNA sequencing to identify the bacterial communities associated with each clay system. Results show that samples decaying on the surface of kaolinite have a lower bacterial diversity than those decaying on the surface of bentonite and montmorillonite, which could explain the limited decay of carcasses deposited on this clay. However, this is not the only role played by kaolinite, as a greater proportion of gram-negative over gram-positive bacteria is observed in this system. Gram-positive bacteria are generally thought to be more efficient at recycling complex polysaccharides such as those forming the body walls of arthropods. This is the first experimental evidence of sediments shaping an entire bacterial community. Such interaction between sediments and bacteria might have contributed to arthropods exquisite preservation and prevalence in kaolinite-rich Lagerstatten of the Cambrian Explosion.

paleontology↗

New opabiniid diversifies the weirdest wonders of the euarthropod lower stem group

Once considered weird wonders of the Cambrian, the emblematic Burgess Shale animals Anomalocaris and Opabinia are now recognized as lower stem-group euarthropods. Anomalocaris and its relatives (radiodonts) had a worldwide distribution and survived until at least the Devonian, whereas - despite intense study - Opabinia remains the only formally described opabiniid to date. Here we reinterpret a fossil from the Wheeler Formation of Utah as a new opabiniid, KUMIP 314087. By visualizing the sample of phylogenetic topologies in treespace, our results fortify support for the position of KUMIP 314087 beyond the nodal support traditionally applied. Our phylogenetic evidence expands opabiniids to multiple Cambrian Stages spanning approximately five million years. Our results underscore the power of treespace visualization for resolving imperfectly preserved fossils and expanding the known diversity and spatiotemporal ranges within the euarthropod lower stem group. Additional noteThis work contains a new biological name. New names in preprints are not considered available by the ICZN. To avoid ambiguity, the new biological name is not included in this preprint, and the specimen number (KUMIP 314087) is used as a placeholder. O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=150 SRC="FIGDIR/small/434726v1_ufig1.gif" ALT="Figure 1"> View larger version (98K): org.highwire.dtl.DTLVardef@e770aaorg.highwire.dtl.DTLVardef@95bbd3org.highwire.dtl.DTLVardef@5e460eorg.highwire.dtl.DTLVardef@1494152_HPS_FORMAT_FIGEXP M_FIG O_FLOATNOCover image.C_FLOATNO Artistic reconstruction of the new opabiniid from the Wheeler Formation, Utah, USA (Cambrian: Drumian). Artwork by F. Anthony. C_FIG

paleontology↗