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      Two new species of Tasiocera Skuse from Baltic amber (Diptera, Limoniidae)

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          Abstract

          The paper presents very rare fossil record of crane flies. Inclusions in Baltic amber have documented the second evidence of the existence of the genus Tasiocera (Diptera: Limoniidae: Chioneinae) in ancient epochs of Earth’s history. Hypotheses were also introduced regarding the environmental preferences of fossil Dasymolopilus in relation to modern representatives of the subgenus. The genus is numerous in species and widespread in the modern fauna, while only one species, Tasiocera ( Dasymolophilus) circumcincta, has been known from the fossil record to date. The paper presents an additional description and graphic documentation of this species based on new materials. The discovery of two other species Tasiocera ( Dasymolophilus) gorskii sp. nov. and Tasiocera ( Dasymolophilus) baltica sp. nov. in Eocene resins documents the occurence of Tasiocera since Eocene. Interestingly, only subgenus Dasymolophilus is represented both in extinct and extant fauna while subgenus Tasiocera is not known from the fossil record. The new discovery is very significant, and the result of the study adds a brick to our understanding of the evolution of this group of insects and their habitat.

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          Dicranoptycha Osten Sacken, 1860 (Diptera, Limoniidae) from the earliest Cenomanian Burmese amber

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            Future behavior of wind wave extremes due to climate change

            Extreme waves will undergo changes in the future when exposed to different climate change scenarios. These changes are evaluated through the analysis of significant wave height (Hs) return values and are also compared with annual mean Hs projections. Hourly time series are analyzed through a seven-member ensemble of wave climate simulations and changes are estimated in Hs for return periods from 5 to 100 years by the end of the century under RCP4.5 and RCP8.5 scenarios. Despite the underlying uncertainty that characterizes extremes, we obtain robust changes in extreme Hs over more than approximately 25% of the ocean surface. The results obtained conclude that increases cover wider areas and are larger in magnitude than decreases for higher return periods. The Southern Ocean is the region where the most robust increase in extreme Hs is projected, showing local increases of over 2 m regardless the analyzed return period under RCP8.5 scenario. On the contrary, the tropical north Pacific shows the most robust decrease in extreme Hs, with local decreases of over 1.5 m. Relevant divergences are found in several ocean regions between the projected behavior of mean and extreme wave conditions. For example, an increase in Hs return values and a decrease in annual mean Hs is found in the SE Indian, NW Atlantic and NE Pacific. Therefore, an extrapolation of the expected change in mean wave conditions to extremes in regions presenting such divergences should be adopted with caution, since it may lead to misinterpretation when used for the design of marine structures or in the evaluation of coastal flooding and erosion.
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              The taphonomy of colour in fossil insects and feathers

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                Author and article information

                Contributors
                ikania@ur.edu.pl
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                3 January 2024
                3 January 2024
                2024
                : 14
                : 350
                Affiliations
                [1 ]Institute of Biology, University of Rzeszów, ( https://ror.org/03pfsnq21) Rzeszów, Poland
                [2 ]GRID grid.413454.3, ISNI 0000 0001 1958 0162, Institute of Systematics and Evolution of Animals, , Polish Academy of Sciences, ; Kraków, Poland
                Author information
                http://orcid.org/0000-0002-2325-4308
                http://orcid.org/0009-0001-1316-7008
                http://orcid.org/0000-0002-0453-550X
                http://orcid.org/0000-0001-5685-891X
                Article
                51033
                10.1038/s41598-023-51033-z
                10764351
                38172206
                3222fd3b-a0a1-4fcf-82cd-a7810ef33c3f
                © The Author(s) 2024

                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
                : 18 July 2023
                : 29 December 2023
                Funding
                Funded by: National Science Centre, Poland. Polish Academy of Sciences, Kraków
                Award ID: Grant No. 2020/37/B/NZ8/03042
                Award Recipient :
                Categories
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                © Springer Nature Limited 2024

                Uncategorized
                evolution,environmental sciences
                Uncategorized
                evolution, environmental sciences

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