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A review of the Rissoinidae and Zebinidae (Caenogastropoda, Littorinimorpha) from the Circumarabian Seas, with the description of six new species
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RBINS Staff Publications 2024
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A cooperative game-theoretic framework for negotiating marine spatial allocation agreements among heterogeneous players.
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RBINS Staff Publications 2017
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Consistent patterns of spatial variability between NE Atlantic and Mediterranean rocky shores
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RBINS Staff Publications 2017
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Geographic patterns of biodiversity in European coastal marine benthos
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RBINS Staff Publications 2017
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Essence of the patterns of cover and richness of intertidal hard bottom communities: a pan-European study.
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RBINS Staff Publications 2017
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The role of physical variables in biodiversity patterns of intertidal macroalgae along European coasts.
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RBINS Staff Publications 2017
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Age of mud breccia from mud volcanoes in Academician Ridge, Lake Baikal
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Lake Baikal is the only freshwater reservoir on Earth with gas-hydrate accumulations in its bottom sediments, partly due to the activity of mud volcanoes. This paper describes a group of mud volcanoes recently discovered on the slope of the Academician Ridge between the northern and central Lake Baikal basins. Our analysis of diatom skeletons in the mud breccia sampled from the study area shows a high abundance of Cyclotella iris et var. These extinct species were also discovered in a core sample from BDP-98 borehole. Based on the biostratigraphic and seis-mostratigraphic correlations, the age of the mud breccia in the studied mud volcanoes ranges from the Late Miocene to the Early Pliocene (4.6 to 5.6 Ma). The correlations suggest that the material originated from a depth of less than 310 m below the lake bottom.
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RBINS Staff Publications 2017
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High-amplitude lake-level changes in tectonically active Lake Issyk-Kul (Kyrgyzstan) revealed by high-resolution seismic reflection data
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A total of 84 seismic profiles, mainly from the western and eastern deltas of Lake Issyk-Kul, were used to identify lake-level changes. Seven stratigraphic sequences were reconstructed, each containing a series of delta lobes that were formed during former lake-level stillstands or during slow lake-level increase or decrease. The lake level has experienced at least four cycles of stepwise rise and fall of 400202fm or more. These fluctuations were mainly caused by past changes in the atmospheric circulation pattern. During periods of low lake levels, the Siberian High was likely to be strong, bringing dry air masses from the Mongolian steppe blocking the midlatitude Westerlies. During periods of high lake levels, the Siberian High must have been weaker or displaced, and the midlatitude Westerlies could bring moister air masses from the Mediterranean and North Atlantic regions.
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RBINS Staff Publications 2017
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A fossil heron from the early Oligocene of Belgium : the earliest temporary well-constrained record of the Ardeidae
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We describe the earliest temporally well-constrained fossil that can be assigned to the Ardeidae (herons), from the lowermost Oligocene (32.0–33.0 million years ago) of Belgium. The specimen, a partial tarsometatarsus, belongs to a small species and is described as Proardea? deschutteri n. sp. It exhibits the characteristic tarsometatarsus morphology found in extant heron species, but a confident assignment to one of the ardeid subclades is not possible and even the assignment of the new fossil species to the crown group (the clade including the extant species) cannot be established. The fossil indicates a divergence of herons from their sister taxon by at least the earliest Oligocene, and current paleontological data suggest that herons arrived in Europe shortly after a major faunal turnover at the Eocene/Oligocene boundary. We consider that dispersal is the likely reason for the sudden appearance of herons in the earliest Oligocene of Europe but it is uncertain from where exactly this took place, with Asia and Africa being among the candidate areas.
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RBINS Staff Publications 2018
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Letters to the twenty-first century botanist. Second series:“what is a seed?”–3. How did we get there? Palaeobotany sheds light on the emergence of seed
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This paper discusses the main steps leading to the acquisition, during the Palaeozoic, of the seed habit. The earliest spermatophytes originated in the Late Devonian and produced small cupulate ovules characterized by an elaborated sporangial apex involved in pollination. The diversification of ovules during the Carboniferous led to a wider range of sizes and shapes, and an increasing importance of the integument. The earliest seeds containing embryos are reported in Carboniferous coniferophytes.
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RBINS Staff Publications 2018