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Article Reference Weather and climate related spatial varability of high turbidity areas in the North Sea and the English Channel
Located in Library / Pending old publications
Article Reference Limits of calcium isotopes diagenesis in fossil bone and enamel
Diagenesis has been recognized for decades to significantly alter the trace elements biogenic signatures in fossil tooth enamel and bone that are routinely used for paleobiological and paleoenvironmental reconstructions. This signature is modified during diagenesis according to a complex continuum between two main processes, addition and substitution. For an additive-like, or early diagenesis, the trace elements biogenic profiles can be restored by leaching secondary minerals, but this technique is inefficient for a substitutive-like, or extensive diagenesis for which secondary trace elements are incorporated into the biogenic mineral. This scheme is however unclear for Ca, the major cation in tooth enamel and bone hydroxylapatite, whose stable isotope composition (δ44/42Ca) also conveys biological and environmental information. We present a suite of leaching experiments for monitoring δ44/42Ca values in artificial and natural fossil enamel and bone from different settings. The results show that enamel δ44/42Ca values are insensitive to an additive-like diagenesis that involves the formation of secondary Ca- carbonate mineral phases, while bone shows a consistent offset toward 44Ca-enriched values, that can be restored to the biogenic baseline by a leaching procedure. In the context of a substitutive-like diagenesis, bone exhibits constant δ44/42Ca values, insensitive to leaching, and shows a REE pattern symptomatic of extensive diagenesis. Such a REE pattern can be observed in fossil enamel for which δ44/42Ca values are still fluctuating and follow a trophic pattern. We conclude that Ca isotopes in fossil enamel are probably not prone to extensive diagenesis and argue that this immunity is due to the very low porosity of enamel that cannot accommodate enough secondary minerals to significantly modify the isotopic composition of the enamel Ca pool.
Located in Library / RBINS Staff Publications 2023
Article Reference Taxonomic Revision of the Genus Trictenotoma Gray, 1832 (Coleoptera: Trictenotomidae). Part 3 – Species from the Philippine Archipelago, with Description of a New Species
Located in Library / RBINS Staff Publications 2021
Article Reference Food nutrient availability affects epibiont prevalence and richness in natural Daphnia populations
Located in Library / RBINS Staff Publications 2020
Article Reference How atmospheric forcing resolution impacts storm surge model results: Insights from Storm Xaver in the North Sea-Scheldt estuary continuum
Estuaries are particularly vulnerable to flooding from storm surges, a risk worsened by climate change. While numerical models are essential for flood risk management, most storm surge models rely on atmospheric forcing data with coarse spatial (tens of kilometers) and temporal (hours) resolutions—significantly lower than the model’s own grid resolution. This mismatch may compromise prediction accuracy. This study evaluates the impact of the spatial and temporal resolution of atmospheric forcing data on storm surge modeling within the Scheldt river-estuary-North Sea continuum for the record-breaking Storm Xaver (December 2013). Atmospheric forcings were incorporated at spatial resolutions ranging from 2 km to 30 km and at temporal resolutions from 15 min to 6 h. Using an unstructured-mesh multiscale hydrodynamic model, we assessed how these variations influenced the accuracy of storm surge simulations. Our findings indicate that spatial resolution has the greatest influence on model performance, with finer resolutions (2–5 km) improving peak surge predictions in estuarine areas. Temporal resolution enhancements provide additional benefits, but only when combined with high spatial resolution. The impact of temporal refinement diminishes rapidly as spatial resolution coarsens beyond 10 km. Notably, the timing of peak surges remains stable across all resolution combinations. The best results are obtained with 2 km and 15 min atmospheric forcing resolution, while 5 km spatial resolution also shows good performance. This study underscores the importance of aligning atmospheric forcing resolution with the hydrodynamic model’s spatial scale to achieve optimal accuracy in storm surge predictions within this estuary.
Located in Library / RBINS Staff Publications 2026
Article Reference A trait-based framework to identify North Sea fauna vulnerable to underwater noise
In the absence of an internationally coordinated management strategy, continued exploitation of the North Sea is expected to exacerbate underwater radiated noise (URN), heightening risks of adverse impacts on marine life. Identifying indicator species and their habitats is a fundamental step in the EU framework for setting a scientifically grounded underwater noise limit value (UNLV). While past research has primarily emphasized marine mammals, there is an increasing effort to highlight that the impacts of URN extend to fishes and invertebrates. To support indicator species selection in the North Sea for URN risk assessment, a trait-based vulnerability scoring system for marine mammals, fishes and invertebrates was developed. Each scoring system evaluates multiple attributes related to a species' capacity to detect and produce sound, as well as the documented impacts from both impulsive and continuous anthropogenic noise, and highlights species of particular concern and socio-ecological significance. Five potential indicator species were identified from each of the three taxonomic groups (marine mammals, fishes and invertebrates) for URN risk assessment. The proposed vulnerability scoring system serves as an adaptive framework, open to iterative refinement as bioacoustics knowledge advances. Although data gaps persist, the establishment of regional UNLV to safeguard vulnerable species should not be delayed. By linking URN exposure with key habitats of identified indicator species, this approach facilitates an ecosystem-based management of URN in the North Sea and provides a transferable framework for other regions.
Located in Library / RBINS Staff Publications 2026
Article Reference Revision of the longirostrine crocodylian Thoracosaurus isorhynchus from the Maastrichtian–Danian of northwestern Europe
A highly debated topic in eusuchian systematics has been the placement of “thoracosaurs,” an assemblage of Cretaceous–Paleogene longirostrine crocodylians from Europe and North America. The position of “thoracosaurs” varies from one study to the next, from being the sister taxon of the extant Gavialis to being excluded from the crown group Crocodylia entirely. Despite these issues, “thoracosaurs” have been understudied, with many taxa suffering from incomplete or outdated descriptions and dubious taxonomic assignment. Here, we provide a comprehensive study of Thoracosaurus isorhynchus from Maastrichtian–Danian deposits of northwestern Europe. We present and describe new material from the type locality of T. isorhynchus. In addition, we redescribe and figure the lectotype and paralectotypes of the species, as well as the material from the Maastrichtian type area, the Netherlands. Moreover, comparison of T. isorhynchus with the type material of Thoracosaurus “scanicus” of the Danian of southern Sweden indicates that the latter might be a junior synonym of T. isorhynchus, suggesting the survival of this species across the Cretaceous–Paleogene boundary. An array of phylogenetic analyses points to a close relationship between T. isorhynchus and the Cenomanian Portugalosuchus azenhae. This implies an early emergence of “thoracosaurs” and causes extensive ghost lineages within Gavialoidea, highlighting the stratigraphic inconsistency of this group and a need for a thorough revision of other “thoracosaurs.”
Located in Library / RBINS Staff Publications 2026
Incollection Reference Shrimp and fish: a unique mixture of a locally produced fish sauce in Roman Harfleur (Normandy, France)
Located in Library / RBINS Staff Publications 2026
Article Reference Carboniferous fossils enlighten the systematics and evolution of Hemiptera
Fossils are witnesses to the evolutionary processes undergone by living lineages. The earliest occurrence of clades provides rich insights into the timing of diversification of lineages and better delimits the groups that compose them. Hemiptera are a remarkable order within the insects due to their high morphological and ecological diversity. However, our understanding of the early evolution of this group remains hampered by the lack of early hemipteran occurrences. In this study we investigate the earliest Carboniferous occurrences of Hemiptera, taking advantage of the redescription of known specimens, and describe three new key hemipteran fossils. We provide thorough taxonomic assessments to describe the earliest occurrences of the Auchenorrhyncha and Sternorrhyncha lineages that constitute major branches in the Hemiptera tree of life. These new occurrences sharpen the delimitations within the classification of Hemiptera and enable better understanding of forewing venation evolution within this hyper-diverse insect order. The following new taxa are described: Protoprosbolomorpha infraorder nov. for Protoprosbole straeleni Laurentiaux, Carbonaturidae fam. nov., Carbonatura oudardi gen. et sp. nov. and Carbopsyllidium minutum gen. et sp. nov.
Located in Library / RBINS Staff Publications 2026
Article Reference Gekko (Gekko) , a new dark-colored tokay gecko from the Thai-Malay border (Squamata, Gekkonidae)
We describe Gekko dam sp. nov. based on type specimens from a limestone hill in Palian District, Trang Province, southern peninsular Thailand. The new species is also found in Satun Province, southern peninsular Thailand, and in Perlis State, northwestern Peninsular Malaysia. A member of the subgenus Gekko, it differs from all currently recognized Gekko species by the following combination of morphological characters and pattern: maximal known snout-vent length of 149.1 mm, lack of contact between nostrils and rostral, 21–24 interorbital scales between supraciliaries, 72–83 scale rows around midbody, 12–14 dorsal tubercle rows at midbody, 26–28 ventral scale rows at midbody, 22 precloacal pores in males, two postcloacal tubercles on each side of the base of the tail, 14–17 subdigital lamellae on 1st toe and 19–21 on 4th toe, a Y-shaped mark on head, white spots on head, dark grey to black dorsal background with four regular bands of contrasting white spots on dorsum between limb insertions, throat and venter white with orange patches, and a copper iris.
Located in Library / RBINS Staff Publications 2026