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      A continuous fish fossil record reveals key insights into adaptive radiation

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          Abstract

          Adaptive radiations have been instrumental in generating a considerable amount of life’s diversity. Ecological opportunity is thought to be a prerequisite for adaptive radiation 1 , but little is known about the relative importance of species’ ecological versatility versus effects of arrival order in determining which lineage radiates 2 . Palaeontological records that could help answer this are scarce. In Lake Victoria, a large adaptive radiation of cichlid fishes evolved in an exceptionally short and recent time interval 3 . We present a rich continuous fossil record extracted from a series of long sediment cores along an onshore–offshore gradient. We reconstruct the temporal sequence of events in the assembly of the fish community from thousands of tooth fossils. We reveal arrival order, relative abundance and habitat occupation of all major fish lineages in the system. We show that all major taxa arrived simultaneously as soon as the modern lake began to form. There is no evidence of the radiating haplochromine cichlid lineage arriving before others, nor of their numerical dominance upon colonization; therefore, there is no support for ecological priority effects. However, although many taxa colonized the lake early and several became abundant, only cichlids persisted in the new deep and open-water habitats once these emerged. Because these habitat gradients are also known to have played a major role in speciation, our findings are consistent with the hypothesis that ecological versatility was key to adaptive radiation, not priority by arrival order nor initial numerical dominance.

          Abstract

          This study presents a continuous fossil record, extracted from a series of sediment cores, that shows how haplochromine cichlids came to dominate the fish fauna of Lake Victoria in Africa.

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          THE INTCAL20 NORTHERN HEMISPHERE RADIOCARBON AGE CALIBRATION CURVE (0–55 CAL kBP)

          Radiocarbon ( 14 C) ages cannot provide absolutely dated chronologies for archaeological or paleoenvironmental studies directly but must be converted to calendar age equivalents using a calibration curve compensating for fluctuations in atmospheric 14 C concentration. Although calibration curves are constructed from independently dated archives, they invariably require revision as new data become available and our understanding of the Earth system improves. In this volume the international 14 C calibration curves for both the Northern and Southern Hemispheres, as well as for the ocean surface layer, have been updated to include a wealth of new data and extended to 55,000 cal BP. Based on tree rings, IntCal20 now extends as a fully atmospheric record to ca. 13,900 cal BP. For the older part of the timescale, IntCal20 comprises statistically integrated evidence from floating tree-ring chronologies, lacustrine and marine sediments, speleothems, and corals. We utilized improved evaluation of the timescales and location variable 14 C offsets from the atmosphere (reservoir age, dead carbon fraction) for each dataset. New statistical methods have refined the structure of the calibration curves while maintaining a robust treatment of uncertainties in the 14 C ages, the calendar ages and other corrections. The inclusion of modeled marine reservoir ages derived from a three-dimensional ocean circulation model has allowed us to apply more appropriate reservoir corrections to the marine 14 C data rather than the previous use of constant regional offsets from the atmosphere. Here we provide an overview of the new and revised datasets and the associated methods used for the construction of the IntCal20 curve and explore potential regional offsets for tree-ring data. We discuss the main differences with respect to the previous calibration curve, IntCal13, and some of the implications for archaeology and geosciences ranging from the recent past to the time of the extinction of the Neanderthals.
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            On the Relationship between Abundance and Distribution of Species

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              Ecological studies in tropical fish communities

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                Author and article information

                Contributors
                nare.ngoepe@eawag.ch
                Journal
                Nature
                Nature
                Nature
                Nature Publishing Group UK (London )
                0028-0836
                1476-4687
                4 October 2023
                4 October 2023
                2023
                : 622
                : 7982
                : 315-320
                Affiliations
                [1 ]Aquatic Ecology and Evolution, Institute of Ecology and Evolution, University of Bern, ( https://ror.org/02k7v4d05) Bern, Switzerland
                [2 ]Department of Fish Ecology and Evolution, EAWAG, Swiss Federal Institute for Aquatic Science and Technology, ( https://ror.org/00pc48d59) Kastanienbaum, Switzerland
                [3 ]Tanzania Fisheries Research Institute (TAFIRI), ( https://ror.org/00h98p168) Dar es Salaam, Tanzania
                [4 ]Institute of Plant Sciences, University of Bern, ( https://ror.org/02k7v4d05) Bern, Switzerland
                [5 ]Geoecology, Department of Environmental Sciences, University of Basel, ( https://ror.org/02s6k3f65) Basel, Switzerland
                [6 ]Center for Water Infrastructure and Sustainable Energy (WISE) Futures, Nelson Mandela African Institution of Science and Technology, ( https://ror.org/041vsn055) Arusha, Tanzania
                [7 ]GRID grid.5734.5, ISNI 0000 0001 0726 5157, Institute of Geography & Oeschger Centre for Climate Change Research, University of Bern, ; Bern, Switzerland
                [8 ]GRID grid.5734.5, ISNI 0000 0001 0726 5157, Institute of Geological Sciences & Oeschger Centre for Climate Change Research, University of Bern, ; Bern, Switzerland
                [9 ]Aquatic Ecology, University of Vic - Central University of Catalonia, ( https://ror.org/006zjws59) Vic, Spain
                Author information
                http://orcid.org/0000-0002-2367-4943
                http://orcid.org/0000-0002-2100-9181
                http://orcid.org/0000-0002-0241-1685
                http://orcid.org/0000-0002-3957-5835
                http://orcid.org/0000-0002-9902-8120
                http://orcid.org/0000-0001-9089-704X
                Article
                6603
                10.1038/s41586-023-06603-6
                10567567
                37794187
                e9ad4ec6-7117-405d-b5b1-4270d330ff2e
                © The Author(s) 2023

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 14 March 2023
                : 1 September 2023
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                © Springer Nature Limited 2023

                Uncategorized
                evolutionary ecology,palaeontology
                Uncategorized
                evolutionary ecology, palaeontology

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