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Listen to the talks at the Geo-Colloquium
The colloquium is held during the lecture period on Wednesdays between 14:15 and 15:30. Please find the upcoming colloquium talks in the schedule.
Contact: Dr. Philipp Sacher
Geo4Göttingen 2025 (2024-12-11, DB)
We are excited to invite you to Geo4Göttingen 2025, a unique joint conference hosted by the University of Göttingen on 14–18 September 2025 in collaboration with four leading scientific societies: the German Geological Society (DGGV), the German Society for Geomorphology (DGGM), the German Mineralogical Society (DMG), and the Paläontologische Gesellschaft (PalGes). This group of four mirrors the composition of Göttingen´s Faculty for Geoscience and Geography but does not constrain the scope of the meeting. We are organizing the conference in close cooperation with the Umbrella Organization of Geosciences in Germany (DVGeo) and aim for the event to cover a wide range of topics, from outer space to crystal lattices and from deep time to femtoseconds. Under the theme Geo4Change - Earth, Life, Climate, Resources, Materials – this conference will highlight some of the most pressing challenges of our time and discuss interdisciplinary solutions. From the dynamic changes shaping our planet to the critical resources that sustain life, we are at a pivotal moment where science must rise to meet global environmental, societal, and technological demands. This year's event is designed to foster collaboration across geosciences, emphasizing innovative approaches to the complex problems we face—whether they relate to climate change, sustainable and innovative use of materials, or the future of Earth's ecosystems. Join us in Göttingen for inspiring discussions, cutting-edge research presentations, and the opportunity to contribute to shaping a better future through geoscience. We look forward to welcoming you to Geo4Göttingen 2025! Cordially, Jonas Kley & the Geo4Göttingen 2025 organizers Click on the image to go to the conference website:
The mystery of Uruguay’s amethyst geodes (2024-10-01, DB)
Amethyst is a violet variety of quartz which has been used as a gemstone for many centuries and is a key economic resource in northern Uruguay. Geodes are hollow rock formations often with quartz crystals, such as amethyst, inside. Amethyst geodes in Uruguay have been found in cooled lava flows, which date from the original breakup of the supercontinent Gondwana around 134 million years ago. However, their formation has remained a mystery. So, a research team led by the University of Göttingen investigated using cutting-edge techniques. The researchers discovered that the amethyst geodes formed at unexpectedly low crystallisation temperatures of just 15 to 60 °C. Taken with their other results, researchers were able to propose a new model to explain their formation. The research was published in the journal Mineralium Deposita. Amethyst has been mined for over 150 years in the Los Catalanes District of Uruguay, where the research was carried out. This is an area renowned for the deep violet colour and high quality of its gems, as well as magnificent giant geodes sometimes over 5 m high. The deposits here have been recognised as one of the top 100 geological heritage sites in the world, highlighting their scientific and natural value. However, limited knowledge of how these geodes formed has made locating them challenging, relying largely on miners’ experience. To address this, researchers conducted extensive geological surveys across more than 30 active mines, analysing geode minerals, geode-hosted water, and groundwater. Using advanced techniques like nucleation-assisted microthermometry of initial one-phase fluid inclusion and triple-oxygen-isotope geochemistry, the team uncovered new insights into how these prized geodes formed. As well as finding that the amethyst geodes formed at unexpectedly low crystallisation temperatures, the researchers also showed that the mineralising fluids had the low levels of salinity and proportion of isotopes consistent with water originating from the natural weather cycle, which probably came from groundwater held in nearby rocks. “The precision and accuracy of these new techniques, allowed us to estimate with confidence the temperature and composition of the mineralizing fluids,” said Fiorella Arduin Rode, lead author and PhD researcher at Göttingen University’s Geoscience Centre. “Our findings support the idea that these amethysts crystallised at low temperatures from groundwater-like fluids.” The study proposes a model where mineral phases like amethyst crystallise within volcanic cavities in a dark rock known as basalt, influenced by regional variations in temperature in the Earth’s crust. Arduin Rode adds, "Understanding the conditions for amethyst formation — such as the temperature and composition of the mineralising fluid, as well as the silica source, the timing of the mineralisation, and its relationship with the host rocks — is crucial for unravelling the process. This could significantly improve exploration techniques and lead to sustainable mining strategies in the future.”
Photos: (L) Fiorella Arduin Rode from the University of Göttingen at the Los Catalanes mining area in northern Uruguay. Together with the Ametista do Sul region in southern Brazil, these areas are the world’s leading mining sites for gemstones extracted from volcanic lava, such as amethyst and agate geodes. (R) An amethyst geode from Los Catalanes is processed in preparation for sale. (F. Arduin-Rode).
Arduin-Rode, F., Sosa, G., van den Kerkhof, A., Krüger, Y., Bajnai, D., Pack, A., Di Rocco, T., Oyhantçabal, P., Wemmer, K., Herwartz, D., Klipsch, S., Wiegand, B., Siegesmund, S., & Hueck, M. (2024). World-class amethyst-agate geodes from Los Catalanes, Uruguay: Genetic implications from fluid inclusions and stable isotopes. Mineralium Deposita. 10.1007/s00126-024-01310-2
Iron-Sulfur Minerals Indicate the Earliest Life on Earth (2024-05-21, DB)
Certain minerals in deep-sea hydrothermal vents could indicate bacterial activity from billions of years ago, which is crucial for understanding the origins of life. This discovery was made by the Universities of Tübingen and Göttingen, and their findings have been published in the journal Communications Earth & Environment. Hydrothermal vents have existed for at least 3.77 billion years and could potentially support life on other celestial bodies in our solar system, as the extreme conditions of these systems are believed to be the birthplace of the first organic compounds and life forms. “To understand how life originated, we aim to trace the evolution of microorganisms back billions of years,” explains doctoral student Eric Runge. Researchers search for biosignatures, traces of life, in the oldest rocks on Earth, with pyrite in a distinctive framboidal form being particularly promising. “Framboidal pyrite only forms when magnetite is produced by iron-reducing bacteria,” says Prof. Dr. Andreas Kappler (University of Tübingen). Experiments show that the crystal forms of biologically and non-biologically formed pyrite differ significantly. The study of biosignatures is also relevant to the search for life on other planets. “Hydrothermal vents similar to those in our deep sea might also exist on Saturn's moon Enceladus,” says Prof. Dr. Jan-Peter Duda. Such studies provide a foundation for recognizing potential signs of extraterrestrial life.
Images: ‘Black smokers,’ hydrothermal vents in the deep sea, emit volcanically heated fluids rich in dissolved metals and sulfur. These environments are oases of microbial activity in the deep sea (MARUM).
Runge, E., Mansor, M., Chiu, T. H., Shuster, J., Fischer, S., Kappler, A., & Duda, J.-P. (2024). Hydrothermal sulfidation of biogenic magnetite produces framboid-like pyrite. Communications Earth & Environment, 5(1), 252. 10.1038/s43247-024-01400-z
Study demonstrates the biological origin of 3.5 billion-year-old carbonaceous matter (2024-02-21, DB)
To learn about the first organisms on our planet, researchers must analyze the rocks of early Earth. These are only found at a few locations worldwide. The Pilbara Craton in Western Australia is one of these rare sites: here, rocks dating back approximately 3.5 billion years emerge, containing traces of the microorganisms that lived at that time. A research team led by the University of Göttingen now provides new insights into the formation and composition of this ancient biomass, offering a glimpse into the earliest ecosystems of Earth. Using high-resolution techniques such as Nuclear Magnetic Resonance Spectroscopy (NMR) and Near-Edge X-ray Absorption Fine Structure Spectroscopy (NEXAFS), the researchers examined carbonaceous particles found in barite rocks. This enabled them to gain crucial information about the structure of the microscopic particles and demonstrate their biological origin. It is likely that the particles sedimented in the water body of a volcanic crater (caldera) at that time. Additionally, a portion apparently was transported and altered by hydrothermal waters in the subsurface of the volcanic system, indicating a turbulent deposition history. Furthermore, from the analysis of various carbon isotopes, the researchers concluded that different types of microorganisms already lived in the vicinity of volcanic activity, similar to today's geysers in Iceland or hot springs in Yellowstone National Park. The study not only sheds light on the Earth's past but is also interesting from a methodological perspective. Lead author Lena Weimann from the Geoscience Center at the University of Göttingen explains: "It was very exciting for us to combine various high-resolution techniques and derive connections to the origin and deposition history of organic particles. As our findings demonstrate, even extremely old material can yield original signals of the first organisms."
Photos: (L) Rock exposed at the surface of the Pilbara Craton: gray barite rock below, with stromatolites above, reddened by oxidation. (R) Lena Weimann in the lab (J.-P. Duda & G. Hundertmark).
Weimann, L., Reinhardt, M., Duda, J.-P., Mißbach-Karmrodt, H., Drake, H., Schönig, J., Holburg, J., Andreas, L. B., Reitner, J., Whitehouse, M. J., & Thiel, V. (2024). Carbonaceous matter in ∼3.5 Ga black bedded barite from the Dresser Formation (Pilbara Craton, Western Australia) – Insights into organic cycling on the juvenile Earth. Precambrian Research, 403, 107321. 10.1016/j.precamres.2024.107321
Inauguration of the new GoeLEM Equipment Center (2024-02-21, DB)
The Faculty of Geosciences and Geography is renowned for its expertise and excellent analytical equipment, utilized by numerous researchers at the University of Göttingen and beyond. Over the past three years, the Geoscience Center at the University of Göttingen has established a modern infrastructure for an equipment center dedicated to light and electron microscopy. The facility includes an electron microprobe, a high-resolution scanning electron microscope, and additional electron and light microscopes. In addition to imaging techniques and electron diffraction, the focus of methodological application lies in the quantitative micro-area analysis, encompassing natural samples such as minerals, as well as modern materials. The equipment center provides researchers from all faculties with analytical opportunities for the high-resolution characterization of materials and their chemical properties down to the sub-nanometer range. The total costs amounted to approximately three million euros, with the Lower Saxony Ministry of Science and Culture supporting the investment with around 1.2 million euros. The installation of the latest equipment, a field emission scanning electron microscope, is now complete. Thus, the Goettingen laboratory for correlative Light and Electron Microscopy (GoeLEM) is fully operational and ready for use. Let's celebrate! For this reason, a festive colloquium took place on February 7th. Metin Tolan (President of the Georg-August University), MD Rüdiger Eichel (Head of the Department of Research, Innovation, Europe at the MWK), Prof. Dr. Christoph Dittrich (Dean of the Faculty of Earth Sciences and Geography), and Prof. Dr. Andreas Pack (Director of the Geological Center) gave speeches. Finally, Prof. Dr. Thomas Müller delivered the keynote speech: "GoeLEM - Visions, Perspectives, and Possibilities of Correlative Electron Optical Analysis." The local newspaper "Göttinger Tageblatt" reported on the event.International Symposium on Quartz and Glass (2024-01-22, DB)
The QUARTZ-2024 symposium will bring together geoscientists, mineralogists, petrologists, material scientists, and sedimentologists, as well as economic and mining geologists and processing engineers with a special interest in quartz and other silica types like chert and glass. The latest results from a broad spectrum of ongoing research on quartz will be presented and discussed. We emphasise the importance and the economical and ecological sustainability of quartz as a resource material for the glass production, because of its particular economic importance in Germany. A panel discussion at the symposium will focus on that theme and will combine geoscientific as well as material scientific aspects. Registration and further information:
New pieces discovered in the cradle of life puzzle (2024-01-22, MR)
An international research team led by Dr. Manuel Reinhardt (University of Göttingen/Linnæus University) unravels new key findings about the earliest life forms on Earth. In rock samples from the Barberton greenstone belt, Republic of South Africa, the researchers were able to find evidence of an unprecedented diverse biological carbon cycle established around 3.42 billion years ago. This proves that ecosystems hosted complex microbial communities already at these ancient times. Microorganisms represent the earliest life forms on our planet, indicated by morphological and geochemical traces preserved in ca. 3.5 billion year old rocks. However, evidence to reconstruct early life on Earth is scarce and often highly disputed. It is still not clear when and where life emerged and when early microbial communities diversified. By analyzing well-preserved carbonaceous matter and associated mineral phases the researchers found geochemical fingerprints of different microbiota, including phototrophs, sulfate reducers, and likely methane cycling microbes. This spectacular finding highlights that ecosystems in the Paleoarchean Era (3.6–3.2 billion years ago) already hosted complex microbial communities. The results have now been published in Precambrian Research. “Our study opens a rare window into early ecosystems on Earth. We did not expect to find traces of so many different metabolisms. It was like finding the needle in the haystack”, says Dr. Manuel Reinhardt, first author of the study. A highlight of the study is the combination of macro- and micro-scale analytical techniques to robustly identify the ancient biosignatures in the rock material. “In early life science, it is crucial to have supporting evidence from various angles to clearly identify indigenous biological traces and distinguish them from potential later contamination”, Dr. Reinhardt adds. “The discovery of organic matter particles in primary pyrite crystals and the direct micro-analysis of carbon and sulfur isotopes therein gave us the rare opportunity to distinguish individual microbial metabolisms”, explains Dr. Henrik Drake, Linnæus University, senior author of the study. “By combining these data with petrographical evidence we were able to pinpoint the roles of different microbes in the cycling of carbon in the Paleoarchean ecosystem”, Reinhardt concludes. “This study marks a significant leap forward in our understanding of the Earth's ancient microbial environments and opens new avenues for future research in the field of paleobiology.”
Photo: Drill core sample from the Barberton greenstone belt used in the study. The dark layers contain carbonaceous matter that originates from Paleoarchean microorganisms (Manuel Reinhardt).
Reinhardt, M., Thiel, V., Duda, J.-P., Hofmann, A., Bajnai, D., Goetz, W., Pack, A., Reitner, J., Schanofski, M., Schönig, J., Whitehouse, M.J. and Drake, H. (2024) Aspects of the biological carbon cycle in a ca. 3.42-billion-year-old marine ecosystem. Precamb. Res., 402, 107289. 10.1016/j.precamres.2024.107289
New study including GZG researchers shed light on unique fibre structure, evolutionary history and combating invasive species (2023-12-14, DB)
Zebra and quagga mussels, which belong to the Dreissenid family, are freshwater invasive species widespread throughout western Europe and North America. They present a significant danger to native ecosystems by competing for resources. Using a fibrous anchor called a byssus, Dreissenid mussels also cause biofouling by attaching persistently to underwater surfaces and for example block the intakes of power stations and water treatment plants. A research team led by McGill University in Canada and Göttingen University in Germany discovered that a rare genetic event, occurring over 12 million years ago, played an important role in shaping one of Europe and Canada’s most damaging invasive species. Their research also sheds light on how mussel fibres could inspire the development of sustainable materials in the future. Their findings were published in PNAS. The researchers collected material from zebra and quagga mussels in Germany and Canada to investigate how these mussels stick to surfaces. Researchers at McGill used a variety of techniques to characterise some of the materials properties of the byssus thread to better understand how this biological material allows the animal to attach itself with such resilience to almost any underwater surface. Researchers in Göttingen identified and sequenced a gene that codes for a byssus thread protein that makes the distinctive silken fibres, performed the structural modelling of the protein and carried out analyses that clarified its evolution. During his involvement in the project Professor Daniel J. Jackson observed Dreissenid mussels in Germany’s Northeimer Seenplatte lakes. He explains, “It was shocking to see how abundant they are there. This shows how invasive the quagga and zebra mussels are, and how they can completely dominate certain habitats.” The researchers discovered that a previously undocumented evolutionary event contributed to Dreissenid mussels’ resilience and success as an invasive species. Jackson explains, "More than 12 million years ago, it is likely that a single bacterium transferred foreign genetic material into a single mussel endowing its descendants with the ability to make these fibres. Given their crucial role in mussel attachment in freshwater habitats, this horizontal gene transfer event supported the harmful global expansion of these mussels.” This research, marking important progress in the understanding of invasive mussels and their attachment mechanisms, could offer potential solutions to mitigate their damaging environmental and economic impact. In addition, the research advances understanding of the mechanisms of biofouling and sheds light on how mussel fibres could inspire the development of sustainable materials. The researchers found that the building blocks of the fibres were massive coiled-coil proteins, the largest ever found. These proteins, structurally similar to those found in human hair, were found to transform into silk-like beta crystallites through the simple application of stretching forces by the mussel during formation. This method of fibre fabrication is much simpler than spider silk formation, potentially offering an easier route toward biotechnological manufacture of sustainable fibres – an industry currently dominated by artificial spider silks. Professor Matthew Harrington, McGill University Department of Chemistry, explains: "Dreissenid byssus fibres, which resemble spider silk structurally, could inspire future development of tough polymer fibres, contributing to more durable and sustainable materials typically used in textiles and technical plastics.”
Photo: Dreissenid byssus morphology. Figure from the manuscript.
Simmons, M., Horbelt, N., Sverko, T., Scoppola, E., Jackson, D. J., Harrington, M. J. (2023) Invasive mussels fashion silk-like byssus via mechanical processing of massive horizontally acquired coiled coils, PNAS, 120, e23119011, 10.1073/pnas.2311901120
Cover of Geochemical Perspective Letters showcases first-author paper by student from the Geobiology Team Göttingen (2023-08-29, DB)
Congratulations to Jorinel Manuel Domingos, an MSc student and a valuable member of the Göttingen Geobiology Group. His first-author publication about pyrite growth has made it to the front cover of the prestigious journal Geochemical Perspective Letters. J.M. Domingos, E. Runge, C. Dreher, T.-H. Chiu, J. Shuster, S. Fischer, A. Kappler, J.-P. Duda, J. Xu, and M. Mansor (2023): Inferred pyrite growth via the particle attachment pathway in the presence of trace metals. Geochemical Perspective Letters, 26, 14-19, 10.7185/geochemlet.2318
Photo: Cover of Vol. 27 of Geochemical Perspective Letters. False colour image of lab-synthesised pyrite crystals with diverse sizes and morphologies. Colours reflect different inferred growth stages: from the green/cyan microframboids to yellow octahedral crystals to red pyrite “roses”. Images such as this and others provide insight into mineral growth via the particle attachment pathway, which affects how trace metal distributions and mineral morphology can be used as biosignatures and environmental proxies
(credit: Jeremiah Shuster)
Jan-Peter Duda awarded visiting professorship at Northwest University (2023-05-15, DB)
We are delighted to announce that Prof. Jan-Peter Duda has been awarded a prestigious visiting professorship at Northwest University (NWU) in Xi'an, PR China, in recognition of his exceptional contributions and expertise in early life and deep-time geobiology. In addition to the visiting professorship, Jan-Peter Duda has been appointed as an overseas academic expert at the 111 Center Early Life & Environments at NWU. The news was officially conveyed by a delegation of esteemed visitors from NWU, which included Prof. Shaocong Lai (Vice President NWU) and Prof. Dongjing Fu. They recently visited Göttingen to personally inform Jan-Peter Duda about the appointment and to discuss future collaborations in research and teaching.
Photos: Pictures of Prof. J.-P. Duda receiving the honors from the delegation of NWU, Prof. Shaocong Lai and Prof. Dongjing Fu (J.-P. Duda).
Renas Koshnaw receives Postdoctoral Researchers International Mobility Experience (PRIME) fellowship from DAAD (2023-03-02, DB)
Renas Koshnaw joined the Göttingen Geoscience Center as a Humboldt Research Fellow in 2019, hosted by Jonas Kley and the structural geology department. Renas was born and raised in Erbil, Kurdistan Region of Iraq. He holds an MSc and PhD from the University of Texas at Austin. His research focuses on the tectonic evolution of the Zagros Mountains and addresses topics ranging from lithosphere-scale geodynamics and thrust belt structure to sediment provenance, transport and deposition. One of his main interests is to constrain how the interplay of tectonic and surface processes has shaped the mountains and their foreland in the course of continental collision. Renas is one of 25 individuals who were selected for the PRIME fellowship 2022/23 out of 133 applicants. He will spend 12 months conducting research abroad at the Massachusetts Institute of Technology in the United States, where he will investigate the fate of the Neotethys oceanic slab located between the Arabian and Eurasian plates. On another note, Renas recently wrote a public outreach article on the geology of the Zagros Mountains and his own research there in the new Kurdistan Chronicle magazine. You will find his contribution on page 45 of the pdf (p. 88 of the magazine). You may also want to check out other aspects of Kurdistan, its nature, culture and people in the new magazine!
Photos: A picture of Renas Koshnaw and the Zagros Mountains (R. Koshnaw).
Cherts record cooling of the Earth over billions of years (2022-12-20, DB)
Researchers from the Sedimentology and Environmental Geology Department analyse oxygen isotopes in 550 million-year-old samples Several billion years ago, the oceans were probably not as hot as often assumed, but were instead at much more moderate temperatures. This is the conclusion of a research team around Jun.-Prof. Michael Tatzel from GZG. The scientists analysed cherts, sedimentary rocks that form from seawater and the remains of silica-secreting creatures. Using these "time capsules", the team showed that the oxygen isotope ratios are determined by the cooling of the solid Earth and depend less on the temperatures of seawater. The results were published in PNAS.How can it be that ancient cherts – between 3.85 and 2.5 billion years old – are so highly enriched with the lighter oxygen isotope (16O)? What information do these valuable time capsules actually record about the history of our Earth? To investigate this decades-old mystery in the geosciences, the research team examined circa 550 million years old cherts from southeast China. These samples document that after the deposition of sedimentary mud, the amorphous precursors of cherts recrystallise hundreds of metres below the Earth's surface, recording temperatures at depth – and not the temperature of the ocean above them. This finding sparked the idea that oxygen isotope ratios could depend on the heat flow from the Earth's interior – a completely new angle on the old mystery. When the flow of heat is higher, the proportion of 16O becomes higher, because recrystallisation takes place at higher temperatures. At the same time, seawater is enriched with 16O. This solves the puzzle of why there is a large proportion of the lighter oxygen isotope in ancient cherts: heat flow on the early Earth was approximately double modern values. The calculated effect of heat flow on oxygen isotopes in cherts also means that the isotopically light Archean cherts are indicative of a temperate to warm climate on early Earth – hot oceans seem very unlikely. This conclusion is central to understanding the evolution of life on the young Earth. These new findings will open the door to some exciting new developments in the coming years, because understanding of the heat flow effect will allow more accurate reconstructions of seawater temperatures in deep geological time. In addition, this work provides the basis for new discoveries about the thermal-and tectonic history of ancient sedimentary basins.
Image: A photo of the 550 million-year-old cherts analysed in the study (M. Tatzel).
Tatzel, M., et al. (2022) Chert oxygen isotope ratios are driven by Earth’s thermal evolution, PNAS, 119(51), e2213076119, 10.1073/pnas.2213076119
Contact: Michael Tatzel
Press release
Five students received the Adolf von Koenen Award (2022-12-08, DB)
Since 2009 the Adolf von Koenen Award has been given every year to outstanding BSc and MSc theses and doctoral dissertations within Earth Sciences. Besides the prestigious distinction, the awardees also receive a financial donation, thanks to the Friends of Geosciences at the University of Göttingen Association. Due to the canceled award ceremony last year, the awardees of 2021 presented their work together with the 2022 awardees during the Nikolauskolloquium.
Image: The Adolf von Koenen-awardees of 2021 and 2022. Right to left: Tom Baumgarten, President of the association “Friends of Geosciences at the University of Göttingen”, Nina Caroline Lindstedt, Anne Friedrich, Yu Pei, Kristina Sass, Dean of Studies Thomas Ptak and Jonas Kley. Awardee Carsten Benner could unfortunately not attend. Photo: L. Leschner
Nina Caroline Lindstedt's work (Bsc 2021) records slow sediment accumulation rates due to global sea level rise and connects the results to coastal protection in a cultural landscape. The work is praised for its outstanding sedimentological and engineering-geological results, rich illustration, and broad methodological approach. Moreover, her work successfully combined geoscientific facts and a cost/benefit analysis in coastal protection. (Supervisor: Dr. Matthias Deicke; co-supervisor: Prof. Dr. Rainer Markgraf)
Anne Friedrich's work (BSc 2022) impresses with a well-structured and clearly communicated presentation of the experimental synthesis of opal. A successful combination of different analytical methods and the resulting data allowed her to gather compelling insights about opal genesis. Her networking and exemplary commitment to public outreach are reflected in the overall high originality of her work. (Supervisor: Dr. Kirsten Techmer, co-supervisor: Prof. Dr. Sharon Webb)
Kristina Sass (MSc 2021), in her impressive, very well-structured, linguistically clean, and perfectly illustrated work, has investigated the Permo-Triassic sandstones of southwestern Germany "by every trick in the book": she compiled existing heavy mineral data and U-Pb dating of zircons, supplemented them with her own analyses and thus created a comprehensive sedimentary history including provenance changes from the Zechstein to the Upper Buntsandstein. She put together the geologically and stratigraphically complex puzzle of what the study area represents using a multi-disciplinary and broad methodology. (Supervisor: Prof. Hilmar von Eynatten; co-supervisor: Dr. István Dunkl)
Carsten Benner (MSc 2022) has investigated recent sediment samples from streams in the „Nagssugtoqidian“ orogenic belt (Greenland, ca. 1870 million years old). He aimed to study the controversial paleo-proterozoic plate tectonics, suggested by minerals of ultra-high pressure metamorphism. After an all-around successful discussion of the topic, he presents the results of his analytically complex investigations. The analyses of nearly 38,000 heavy minerals and 1,800 garnets delivered indications of predominantly high-temperature metamorphism; nevertheless, the presence of minerals of the ultra-high pressure facies could not be excluded completely. The question remains exciting. (Supervisor: Jan Schönig; co-supervisor: Prof. Dr. Hilmar von Eynatten)
Yu Pei's cumulative PhD dissertation – clean, mature, and comprehensively documented and illustrated – is addressed one of the largest global-ecological problems in Earth's history: biological extinction events with bio-geochemical implications, the causes of which remain staggering and speculative. On the example of dynamic carbonate sedimentation around the Permian/Triassic boundary in southern China and the Germanic Basin, she has exhaustively recorded and described the changes from enzymatically-controlled to microbially-controlled carbonate production to organo-mineralization in the Triassic, thus providing another building block for understanding Earth-historical incisions. (Supervisor: Prof. i.R. Dr. Joachim Reitner; co-supervisor: Prof. Dr. Jan-Peter Duda)
Congratulations!