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The most recent publications from the department

A fossil microbial consortium composed of anaerobic fungi and methanogens is described in drill cores of 540 meters depths, and an age of 39 Ma, from the Siljan impact crater. The microbes existed at strict anoxic conditions deep in the bedrock where they produced methane. The anaerobic fungi decomposed oil that are migrating in the crater´s fracture system, and in the process, H2 was produced, which the H2-dependent methanogens used to produce the greenhouse gas methane. Our study show that the crater was inhabited still 300 million years after the actual impact, and probably still is.

Drake, H., Ivarsson, M., Heim, C., Snoeyenbos-West, O., Bengtson, S., Belivanova, V., Whitehouse, M. 2021. Fossilized anaerobic and possibly methanogenesis-fueling fungi identified deep within the Siljan impact structure. Communications Earth & Environment, DOI: 10.1038/s43247-021-00107-9external link

Potpurri av foton och bilder på fossila och nulevande gymnospermer

This article summarizes the diversity of living and extinct gymnosperms or “naked seed-bearing” plants. It provides an introduction to the classification of gymnosperms, their origin and early radiation, and the evolution of key diagnostic characters, such as seeds and pollen. The major orders of gymnosperms are summarized and illustrated in terms of their foliar, wood and reproductive characteristics and their stratigraphic and geographic distribution. The controversy over the relationships between the various gymnosperm orders is outlined in a series of simplified phylogenetic trees. The appearance of key characters is plotted on a chart showing the ranges of the major groups through the geological record. Finally, the economic significance of gymnosperms is outlined—from their importance as timber and paper pulp resources to applications in medicine, foodstuffs and flavourings, and to uses within industry as varnishes, cosmetics, gums, and perfume. The role of gymnosperms as allergens and toxins in the environment is also noted. This is a contribution to the book Encyclopedia of Geology, 2nd Edition.

McLoughlin, S., 2021. History of Life: Plants: Gymnosperms. In: Elias, S. & Alderton, D. (eds), Encyclopedia of Geology, 2nd Edition. Elsevier, Amsterdam, 476–500. https://doi.org/10.1016/B978-0-08-102908-4.00068-0external link

Schematisk bild över hur svamphyfer, sporer och biofilm lever i sprickor, hålor och gångar i djupbergarter.

Paleontology is based on fossils found in sedimentary rocks. Research at the Swedish Museum of Natural History has during the last decade shown that fossils also are found in igneous rock. Such fossils are the fossil record of the deep biosphere. The deep biosphere is today the second largest reservoir of live biomass and prior to plants colonized land the deep biosphere was the largest reservoir of live biomass. This suggests that the deep biosphere played an unrecognized role in the evolution of prokaryotes and eukaryotes. Here, we review the current knowledge of the fossil record of igneous rock, and show that this area of research needs more attention and research in the future for us to fully understand the early development of life.

Ivarsson, M., Drake, H., Neubeck, A., Sallstedt, T., Bengtson, S., Roberts, N.M.W & Rasmussen, B. 2020. The fossil record of igneous rock. Earth Science Reviews, 210, 103342external link.

Remarkably preserved hyolithids with helens and interior soft tissues are reported from the Guanshan Biota (Cambrian, Stage 4) of Shijiangjun section, in Yunnan Province of South China. Extraordinary soft parts preserved in these hyolithids include muscle scars and digestive tracts. Three types of soft part preservation modes are described from the collection: (1) preservation through pyritization, (2) sediment-infilling of guts, and (3) bacterial biofilm pseudomorphs, resulting from endogenous bacterial decay. By comparison with younger hyolithid specimens, the newly collected materials indicate that the gut anatomy of hyolithids was evolutionarily conservative from the early Cambrian through to at least the Ordovician.

Liu, F., Skovsted, C.B., Topper, T.P., & Zhang, Z.-F., 2021. Soft part preservation in hyolithids from the lower Cambrian (Stage 4) Guanshan Biota of South China and its implications. Palaeogeography, Palaeoclimatology, Palaeoecology. https://doi.org/10.1016/j.palaeo.2020.110079external link

From the south polar forests of the mid-Cretaceous (95 million years ago) to the subtropical seas of the Pliocene (4 million years ago), the fossils of the windswept Chatham Islands reveal vivid panoramas of our changing world, and the plants and animals that have inhabited it. The history of fossil exploration on the islands is presented, from the first scientific expeditions of the mid-1800’s to the cutting-edge and profound scientific discoveries of the present. Finally, the book provides an up-to-date overview of the conservation efforts to save some of the world’s rarest animals and plants on this remote volcanic archipelago.

Stilwell, J.D., Mays, C., 2020. Lost World of Rēkohu: Ancient ‘Zealandian’ Animals and Plants of the Remote Chatham Islands. Cambridge Scholars Publishing, Newcastle upon Tyne, 293 pp.

The Permian–Triassic was an interval of nearly 100 million years (299–201 Ma), and included five global mass extinction events, including the largest of all time: the end-Permian event (252.2 Ma). We outline the abundance and distribution changes that these extinction events had on freshwater algae. We identified a distinct province of freshwater algae that stretched across much of Gondwana for most of the Permian, but came to an end at the end-Permian event, along with collapse of the wetland forest biome. Finally, we lay the groundwork for interpreting specific environmental changes from algal abundances, particularly during extinction events.

Mays, C., Vajda, V., McLoughlin, S., 2021. Permian–Triassic non-marine algae of Gondwana—distributions, natural affinities and ecological implications. Earth-Science Reviews. 29 pp. doi: 10.1016/j.earscirev.2020.103382

We describe a new orthothecid hyolith from the early Cambrian of North China (ca 515 million years ago). The new species, Longxiantheca mira, represent one of the most primitive orthothecids known and has a straight cone-shaped shell and a simple disc-like operculum. However, the new specimens preserve imprints of the soft anatomy of the animal and the microscopic structure of the shell. The new finds show that all hyoliths are closely comparable in their soft body anatomy and that the shell of the earliest hyoliths is closely comparable with that of early molluscs, indicating that the groups are closely related.

Li, L., Skovsted, C.B., Yun, H., Betts, M.J. & Zhang, X. 2020. New insight into the soft anatomy and shell microstructures of early Cambrian orthothecids (Hyolitha). Proceedings of the Royal Society B 287: 20201467external link