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Welcome to our lab page!

Image credits: Arkive, O. Sanisidro, Mark Garlick/Science Photo Library, Davide Bonadonna/National Geographic, Christian Jegou/Science Photo Library

The vast majority of Life that existed on our planet is extinct, leaving behind only a handful of surviving lineages with a remarkably conservative molecular makeup: proteins, lipids, and sugars generate all organismal form and function and encode information on physiology and relationships (phylogeny).


Modern biology relies primarily on molecular -omics data to decipher organismal relationships, identify developmental drivers of evolution, and elucidate how organisms interact with each other and their environment. However, integrable biomolecular information has traditionally been assumed to be lost during fossilization, leaving vast gaps in our understanding of the long-term evolutionary drivers shaping the diversity, physiology, and ecology of contemporary life forms. Consequently, our ability to forecast how modern biodiversity will respond to our changing planet in the long run is critically limited by mechanistic inferences from the most recent snapshot of Life’s evolutionary history.

Our lab is based in the Morton K. Blaustein Department of Earth & Planetary Sciences at Johns Hopkins University. We combine expertise from chemistry, biology, and geology to bridge the ‘Molecular Gap’ between Life past and present, ultimately aiming to elucidate the foundational molecular mechanisms of evolution currently concealed within the geological record. We have pioneered the field of Molecular Paleobiology by demonstrating the mechanistic linkage between biomacromolecules and insoluble kerogen preserved in deepest time, and identified the first time-inclusive biomolecular signatures: my team employs experimental, empirical, and theoretical approaches applied to modern and fossil biological samples, curated in museums and collected in the field, to track the alterations of informative biomacromolecules through time and space. By leveraging these insights, we develop molecular phylogenetic and physiological biosignatures that can be integrated across both modern and extinct life forms – generating new primary data that effectively allow us to fill the blank pages in the history of Life.

Our main objective is to investigate evolutionary responses to global environmental and ecological turnovers: using an integrative approach, we target the most critical intervals in Life’s evolutionary history to gather insights that otherwise could not be inferred from the biased sample of lineages surviving into the modern. We not only endeavor to develop solutions for carbon capture inspired by the geological principles of organic matter alteration and storage, but also translate the principles of physiological evolution into models that predict the long-term effects of climate change on today's biodiversity. Hopkins offers an incredibly welcoming and intellectually stimulating environment with complementary expertise and analytical facilities present in Biology, Physics & Astronomy, Chemistry, Engineering, and the Medical School.

Our work spans from prebiotic chemistry to the diversity of Life as we (don't ?) know it, through time and space – we always welcome creative and ambitious ideas, new challenges, and complementary methodological expertise! If this sounds exciting to you, make sure to check out opportunities in our lab and reach out!

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1 Biomolecule fossilization

Our previous research revealed that proteins, lipids, sugars, and certain pigments leave characteristic traces in the fossil record. Different classes of biomolecules undergo characteristic chemical alterations during diagenesis, and tend to transform into more stable compounds which can survive in the geological record.

2 Crosslinking as the mechanism of preservation

During early diagenesis (days to years postmortem), oxidative conditions trigger the formation of Reactive Carbonyl Species (RCS) from lipids and sugars. Oxidative conditions are prevalent in, i.e., fluvial, alluvial, and shallow marine sediments. Lipid- and sugar-RCS show distinct affinities for exposed amino acid residues of omnipresent proteins. Primary targets are nucleophilic amino acid residues, such as arginine, lysine, histidine, and cystein, as well as the protein N-terminus. Observed fossilization reactions include primarily C-C-bond forming reactions, such as transition metal-catalyzed additions. The resulting crosslinking products fall either in the category of Advanced Lipoxidation End Products (ALEs), or Advanced Glycoxidation End Products (AGEs). ALEs and AGEs constitute pre-graphitic insoluble kerogen composed of N-, O-, S-heterocyclic polymers – compounds that are water-insoluble, indigestible to microbes, and energetically stable. There does not seem to be an age limit for the preservation of N-, O-, S-heterocyclic polymers in the geological record!

3 Mineral interactions

The geological product of crosslinking reactions, termed insoluble kerogen, often coordinates transition metals that stabilize the resulting coordination complexes against temperature, pressure, and dissolution stress in the rock record. Such organo-mineral interactions are tissue-specific and can facilitate early diagenetic mineralization of biological materials. Mineralization aids in preserving fragile organic morphologies and storing climate-inactive organic carbon in deep time. We have analyzed more than 300 organic-rich fossils and sediments and are currently expanding this sample to understand the mechanisms involved in phosphatization, pyritization, silicification, and clay mineral precipitation on organic templates. We anticipate that these insights will explain observed biases in the fossil record.

Bridging the ‘Molecular Gap’: biomolecule and biosignature fossilization

We explore to which extent we can truly integrate biological signals encoded in the composition of biomolecules across the physical parameter space. Our lab tackles this challenge by leveraging a combination of experimental, empirical, and theoretical approaches to track the alterations of informative biomacromolecules and the kinetics of biosignature loss as a function of variables (pressure, temperature, etc.) that are relevant to fossilization processes on Earth and elsewhere in the solar system. Our team critically interrogates residual molecular phylogenetic and physiological signals revealed through comparative geochemistry with complementary genomic inferences. We are passionate methodologists, and enjoy developing new protocols, hardware, and data analysis tools for end users interested in the application of our integrative proxies.

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New data, new opportunities: 

the first time-integrative molecular biosignatures and their transformative applications

We apply our different integrative biosignatures to the most challenging open questions in the history of Life. With countless opportunities for transformative applications of the molecular biomineralization, tissue identity, metabolic, and phylogenetic signals, we focus our energy on collecting the first molecular mechanistic insights into evolutionary transitions of primary societal and economic relevance. We find inspiration in our discoveries of mechanisms facilitating molecular preservation in deep time, and adaptations of extinct organisms to carbon fixation during past hot-house climates, and translate these insights into carbon capture and storage technology. We enjoy venturing into uncharted scientific territories and help defining the frontier questions at the interface of the fundamental sciences. Research in our lab is very dynamic and catalyzed by the expertise and ideas of our team members!


Below, you can find a brief introduction of the four biomacromolecular signatures that currently guide our scientific endeavors. In addition, there is a snapshot of current research priorities in the lab related to big questions in astrobiology, prebiotic chemistry, organismal evolution and ecology, biodiversity conservation, and new solutions to carbon capture.

We are incredibly grateful to have brilliant collaborators working with us on our various projects - at Hopkins, in Maryland, and across North America, Australia, South America, Europe, Africa, and Asia!

1 Biomineralization signal


The most prominent signal present in compositional fingerprints of biological materials and their fossilization products identifies templated biomineralization.

In a templated biomineral, coordinating amino acid residues interact with ions of the mineral phase. Non-biomineralized tissues lack mineral-templating proteins and comparable, abundant organo-mineral interactions. This signal preserves accurately even in temperature- and pressure-matured carbonaceous compression fossils from the Precambrian and Cambrian (the time window capturing the diversification of animal skeletons), and accurately distinguishes diagenetically and biologically precipitated minerals.


This proxy has the potential to fundamentally advance our understanding of the nature and evolution of biomineralized tissues, as exemplified in our recent study on eggshell evolution in Nature.

2 Tissue identity signal


The tissue type signal groups tissues by identity based on their specific relative abundancies of proteins, lipids, and sugars. Using a training data set of tissues with known identity, modern and fossil tissues of unknown type can efficiently and non-destructively be characterized.

Different tissues contain characteristic relative amounts of proteins, lipids, and sugars - these compositional fingerprints preserve in the relative amounts of lipoxidation and glycoxidation end products: during early diagenesis, lipids generate characteristic Reactive Carbonyl Species (RCS) which differ from those formed by sugars. Depending on their relative abundance in a tissue, lipid- and sugar-derived RCS crosslink with omnipresent proteins, preserving the original abundance of proteins, lipids, and sugars in the resulting composition of N-, O-, S-heterocyclic polymers in a fossil. This is the second most prominent signal in an animal tissue ChemoSpace.

Being able to unambiguously identify tissues in modern and fossil samples can provide informative characters that help resolving phylogenetic affinities, as shown in our recent study on the phylogenetic affinity of the enigmatic tully monster, published in Geobiology.

3 Metabolic rate signal
















Metabolic stress leaves molecular traces that preserve in deep time and can be quantified to reconstruct the metabolic rates of both extant and extinct animals. Vascularized and cellular tissues, such as bone, preserve metabolic modifications in their proteinaceous phase.​

The metabolic proxy requires the use of homologous structures (due to intraskeletal, tissue-dependent variation). Ongoing research focuses on expanding the phylogenetic applicability of the proxy and discriminating between minute differences in metabolic signals (i.e., true endotherms versus seasonal endotherms).​ Aerobic mitochondrial respiration is far older than the amniote clade, and we thus explore the manifestation of molecular metabolic signals in invertebrates and extinct prokayotes.


Once calibrated based on skeletal metabolic markers of living animals, the abundance of metabolic stress markers can be translated into a metabolic rate (= the amount of oxygen respired relative to the body mass, in one hour of time). 

4 Phylogenetic signal


The phylogenetic signal relies on the compositional differences of amino acid-specific crosslinks in N-, O-, S-heterocyclic polymers. Even though no sequence information can be obtained, the similarity in the relative amino acid composition of homologous tissues provides insights into animal relationships.










Proteins represent translation products of the genetic code. A codon composed of a nucleotide triplet encodes for one out of 21 (for eukaryotes, 22 for all organisms) proteinogenic amino acids. Sequencing modern proteins yields information on organismal relationships, however, diagenetic alteration of peptide bonds during fossilization prevents the sequential cleavage of units through any conventional method. Amine- and thiol-bearing amino acid residues yield diagnostic fossilization products. When comparing N-, O-, S-heterocyclic polymers of the same tissue type and from similar depositional settings, a cluster analysis of the fossil composition reflects organismal relationships. The ability to complement morphological assessments of organismal relationships with molecular data has the potential to resolve controversial nodes in the tree of life.

Space, the final frontier: molecular ecosystems across the solar system and a world before the first complex cells


Past:                How did Life emerge, interact, and evolve on early Earth?

                      What were the selective drivers impacting the composition of pre-cellular ecosystems?

Present & Future: Can we define a fingerprint of Life as we know it to improve our search for Life beyond Earth?

                      Can we constrain plausible chemistries of Life as we don't know it?

Endless forms most beautiful: the many ways Life makes mineral skeletons


Present: What is the relationship between organic template and precipitated biomineral?

Past:     Can we use the biomineralization signal to elucidate when and why the first skeletons evolved?

           How did different biomineralizers react to changing ocean geochemistry (as function of climatic excursions) in the past?

Future:  Can extinct biomineralizers from past hot-house climates inspire carbon capture technology?

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We use extraterrestrial insoluble organic matter imported by carbonaceous meteorites (from Mars, the asteroid belt, and other solar system bodies) as an abiogenic comparison for modern and fossil biogenic organic matter. Statistical analyses of compositional data allow us to define the molecular fingerprint shared by all Life as we know it, and reveal compositional features (apomorphies) that are diagnostic of increasing complexity (ranging from prebiotic mixtures to the first cellular structures preserved in the fossil record on Earth).

We combine techniques allowing for
molecular characterization with in situ observed experimental pressure- and temperature-alteration and theoretical models based on physical variables, to elucidate the origin(s), diversity, and evolution of earliest Life on Earth and elsewhere in the solar system.

Our group explores the foundational mechanisms of templated biomineralization across modern prokaryote and eukaryote systems to reveal how different protein features translate into mineralogies. For modern biominerals, we integrate data on the proteomic make-up, molecular structures, and spatially resolved post-translational modifications in the context of organo-mineral interactions. We experimentally model the pressure- and temperature-alteration (relevant for fossilization processes) of biominerals, and refine our proxies to allow for the integration of data for modern and fossil samples.

We leverage these insights to unravel [1] the
evolutionary mechanisms involved in the independent emergence of biominerals and [2] their clade-specific adaptation potential to long-term climatic and ecological perturbations, with special emphasis on marine calcifiers involved in carbon fixation. Our group translates this information into bio-inspired climate solutions.

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Life finds a way: do physiological and reproductive trade-offs determine the fate of organisms during mass extinctions?


Present:             Can we refine the metabolic proxy and apply it taxon-inclusively from single-celled protists to cellular vertebrate bone?

Past:                 How does the energetic trade-off between metabolism and reproduction relate to major environmental perturbations?

                       How do metabolic changes throughout development/ontogeny impact survival of mass extinction events?

Future:               Can these mechanistic insights improve models predicting the long-term impact of climate change on modern biodiversity?

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Organisms focus their energetic investments either on their metabolism (to grow faster and larger) or reproduction (increased hatchling survival due to parental care). It is the trade-off between metabolism and reproduction that shapes ecological niches and determines extinction susceptibility during times of global perturbations. Until recently, we were unable to gather molecular metabolic and reproductive behavioral data from extinct organisms.

genomic, spatial molecular, and developmental data for living groups with integrable metabolic and reproductive signals from fossils, bridged through experimental fossilization, we work to reveal the evolutionary relationship and selective drivers (environmental, ecological, ontogenetic) of metabolism and reproduction in a comparative framework, across clades. We apply mechanistic insights to more accurately predict the long-term impact of climate change on modern biodiversity.

P/T mass extinction

K/Pg mass extinction

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post - HOP: 2024 and onwards 

Our starting date at Johns Hopkins is July 2024 - Stay tuned for exciting research from the PaLEO Lab!

pre - HOP: 2015 to present

Publications prior to starting my lab at Johns Hopkins

19. Wiemann, J.*, and Heck, P. R. Quantifying the impact of sample, instrument, and data processing on biological signatures detected with Raman spectroscopy. Journal of Raman Spectroscopy, early view. Click here!


18. Wiemann, J.*, Menendez, I.*, Crawford, J.M., Fabbri, M., Gauthier, J.A., Hull, P.M., Norell, M.A., and Briggs, D.E.G. RE: Comment on amniote metabolism and the evolution of endothermy. Nature 621, E4–E6 (2023). Click here! 


17. Tripp, M.*, Wiemann, J., Brocks, J., Mayer, P., Lidgard, S., Schwark, L., and Grice, K. Molecular evidence from coprolites reveals dietary strategies of the Carboniferous Mazon Creek fauna. Biology.

– Invited contribution (special issue). Click here!


16. Norell, M. A., Wiemann, J.*, Menendez, I.*, Fabbri, M.*, Yu, C., Marsicano, C., Pol, D., Moore-Nall, A., Varricchio, D. J., and Zelenitsky, D. Cross-methodological evidence confirms soft eggs in sauropodomorph dinosaurs. Nature. Click here!


15. Wiemann, J.*, Menendez, I., Crawford, J.M., Fabbri, M., Gauthier, J.A., Hull, P.M., Norell, M.A., and Briggs, D.E.G. Fossil biomolecules reveal an avian metabolism in the ancestral dinosaur. Nature, 10.1038/s41586-022-04770-6. Altmetric score: 2033. [Dissertation chapter 3/5] – Most widely shared paleontology paper in 2022. Click here!


14. Wiemann, J.* and Briggs, D.E.G. Raman spectroscopy is a powerful tool in a range of paleobiological applications. Invited contribution, Bioessays, 10.1002/bies.202100070. Altmetric score: 11. Click here!

Preprint: Wiemann, J.* and Briggs, D.E.G. Validation of biosignatures confirms the informative nature of fossil organic Raman spectra. BioRxivClick here!


13. Wiemann, J.*, Crawford, J.M., and Briggs, D.E.G., 2020. Phylogenetic and physiological signals in metazoan fossil biomolecules. Science Advances, 10.1126/sciadv.aba6883. Altmetric score: 103. Click here!


12. Norell, M. A.*, Wiemann, J.*, Fabbri, M.*, Yu, C., Marsicano, C., Pol, D., Moore-Nall, A., Varricchio, D. J., and Zelenitsky, D., 2020. The first dinosaur egg was soft. Nature. Altmetric score: 1439. Click here!


11. McCoy, V. E.*, Wiemann, J.*, Lamsdell, J.C., Whalen, C.D., Lidgard, S., Mayer, P., Petermann, H., and Briggs, D.E.G., 2020. Chemical signatures of soft tissues distinguish between vertebrates and invertebrates from the Carboniferous Mazon Creek Lagerstätte of Illinois. Geobiology, 10.1111/gbi.12397. Altmetric score: 179. Click here!

10. Ibrahim, N., Maganuco, S., Dal Sasso, C., Fabbri, M., Auditore, M., Bindellini, G., Martill, D.M., Wiemann, J., Zouhri, S., Matarelli, D., Unwin, D.M., Joger, U., Amane, A., Jakubczak, J., Bonadonna, D., Lauder, G., and Pierce S., 2020. Tail-propelled aquatic locomotion in a theropod dinosaur. Nature, 10.1038/s41586-020-2190-3. Altmetric score: 3780. Click here!


9. Wiemann, J.*, de Queiroz, K., Rowe, T. B., Planavsky, N. J., Anderson, R. P., Gogarten, J. P., Turner, P. E., and Gauthier, J. A., 2020. Biota. In: de Queiroz, K., Cantino, P. D., and Gauthier, J. A., Editors. Phylonyms: a companion to the PhyloCode. Berkeley, University of California Press - Invited contribution. Registration number: 298. Click here!


8. Wiemann, J.*, de Queiroz, K., Rowe, T. B., Planavsky, N. J., Anderson, R. P., Gogarten, J. P., Turner, P. E., and Gauthier, J. A., 2020. Pan-Biota. In: de Queiroz, K., Cantino, P. D., and Gauthier, J. A., Editors. Phylonyms: a companion to the PhyloCode. Berkeley, University of California Press - Invited contribution. Registration number: 299. Click here!


7. Fabbri, M., Wiemann, J., Manucci, F., Briggs, D.E.G., 2020. 3-D soft tissue preservation revealed in the skin of a non-avian dinosaur. Palaeontology, 10.1111/pala.12470. Altmetric score: 53. Click here!


6. Yang, T.-R., Wiemann, J., Xu, L., Cheng, Y.-N., Wu, X.-C., and Sander, P. M., 2019. Reconstruction of oviraptorid clutches illuminates their unique nesting biology. Acta Palaeontologica Polonica, 10.4202/app.00597.2018. Click here!


5. Wiemann, J.*, Yang, T.R., and Norell, M.A., 2019. Reply to: Egg pigmentation probably has an archosaurian origin. Nature, 10.1038/s41586-019-1283-3. Altmetric score: 35. Click here!


4. Wiemann, J.*, Fabbri, M., Yang, T.R., Stein, K., Sander, P.M., Norell, M.A., and Briggs, D.E.G., 2018. Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 10.1038/s41467-018-07013-3​. Altmetric score: 200. Click here!


3. Wiemann, J.*, Yang, T.R., and Norell, M.A., 2018.  Dinosaur egg color had a single evolutionary origin. Nature, 10.1038/s41586- 018-0646-5. Altmetric score: 1624. Click here!


2. Yang, T.R., Chen, Y.-H., Wiemann, J., Spiering, B., and Sander, P.M., 2018. Fossil eggshell cuticle elucidates dinosaur nesting ecology. PeerJ, 6, p. e5144. Click here!


1. Wiemann, J.*, Yang, T.R., Sander, P.N., Schneider, M., Engeser, M., Kath-Schorr, S., Müller, C.E. and Sander, P.M., 2017. Dinosaur origin of egg color: oviraptors laid blue-green eggs. PeerJ, 5, p.e3706. Altmetric score: 461. Click here!

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Clutch in Paleowonder Museum of Fossil a


Comparable Raman set-up (PC: Tiffany Cassidy)

PaLEO labs (EPS): [1] Spectroscopy lab (UV/Vis/NIR AFM NanoRaman + TERS lab) and [2] chemical-BSL1 wet lab


We are currently setting up our customized Raman microspectrometer and our chemical and microbiological (BSL 1) wet lab - both spaces are located in the Morton K. Blaustein Department of Earth and Planetary Sciences. Raman spectroscopy allows the non-destructive, holistic chemical characterization of complex materials by probing diagnostic interactions between light and molecular or crystal lattice vibrations. Raman spectroscopy is very time-efficient and facilitates the explorative analysis of samples with unknown composition, such as insoluble organic matter preserved in fossils. Large and integrative data sets can be built in a relatively short amount of time for both biological, geological, paleontological, and meteoritic samples. The resulting spectra are particularly suitable for statistical analyses aiding in the search for biosignatures.


After 10 years of exploring different spectrometer types and specifications, I have chosen a Horiba Jobin-Yvon base model which has been tailored to meet our specific analytical needs as cross-disciplinary scientists who work with inherently complex biocomposite materials: our instrument will have three different lasers installed, covering the ultraviolet, visible green, and near-infrared portions of the electromagnetic spectrum! All three lasers can be used in environmental microscopy- or AFM-mode (= atomic force microscopy; for subcellular/micrometer resolution in 2-D, 3-D, or 4-D spatial compound maps). Spatially and temporally resolved compound maps can be collected (label-free!) by taking advantage of the confocal capabilities of our instrument. A hydrothermal diamond anvil cell can be fitted into the microscope framework and allows us to perform experimental pressure-, temperature-, and fluid-based alteration of samples, observable in situ. To capture potentially informative heterogeneities in near-graphitic (high-pressure/high-temperature matured) biomolecule fossilization products, we will use SERS (= surface-enhanced Raman spectroscopy) and TERS (= tip-enhanced Raman spectroscopy) for single-molecule characterization employing combined Plasmonic and Raman effects. The various analytical capabilities in our spectroscopy lab represent the current State-of-the-Art!


Curious? Visitors (bringing interesting samples) are always welcome - we anticipate to be fully operational by spring 2025! Until our spectrometer is set-up and calibrated, my group will be working with the cryo-Raman set-up managed by our wonderful colleagues (PI Natalia Drichko) next door in Physics & Astronomy.

Labs in EPS: Wet geochemistry lab, rock prepation/histology lab, microscopy lab, various mass spectrometry labs ...

Go ahead an explore the details for these various fancy EPS facilities operated by my awesome colleagues on our departmental homepage!

Labs at Hopkins: Biology, Physics & Astronomy, Chemistry, MCP (Materials characterization), Medical School (FAE, Sequencing, etc.)

Go ahead an explore the details for these various Hopkins facilities online (incl. SEM, TEM, FIB/EDS, XRD, Orbitrap MS, NMR, CT, -omics analyses, etc.)!

Museum collections: Smithsonian National Museum of Natural History (Washington DC),

                            American Museum of Natural History (New York)

Follow the links to explore the online catalogues for the NMNH and AMNH collections!

Live animals & conservation in Baltimore: National Aquarium (aquatic metazoans, herpetofauna, tropical mammals and birds)

                                                       The Maryland Zoo in Baltimore (diverse metazoans) 

Follow the links to explore the homepage of the National Aquarium and the Baltimore Zoo!

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The team [We are currently recruiting and evolving - Interested in joining us? Check out opportunities in the lab!]

Principal Investigator: Jasmina Wiemann, PhD 
(Phonetic spelling guide: YahS-Mee-Naa WhEE-Mun)

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I am a Molecular Geo-, Astro-, & Paleobiologist with broad interests in revealing the past, present, and predictable future of Life on Earth and beyond through the exploration and integrative application of molecular biosignatures. I will start as an Assistant Professor in Earth and Planetary Sciences at Johns Hopkins University in July.

My academic journey started at the age of 15, when I was awarded an Excellence Stipend to study Chemistry at the Technical University of Dortmund in Germany. I went on to obtain degrees in the Geosciences (BSc; Honors Program Scholarship) and Organismal and Evolutionary Biology (MSc; Honors Program Scholarship) at the University of Bonn (Germany). During my MPhil and PhD at Yale University in the United States, I combined these disciplines to actively develop the field of Molecular Paleobiology by mechanistically linking informative biomacromolecules to insoluble kerogen preserved in the geological record. My dissertation yielded more than 19 publications (incl. 9x Nature, Science Adv, Nature Comms) demonstrating the preservation of integrative molecular biosignatures in deep time. After graduating, I held Trimble & Barr Postdoctoral Fellowships at Caltech, allowing me to focus on the preservation kinetics and macroevolutionary applications of biological information in terrestrial and extraterrestrial insoluble kerogen. Supported by an Agouron Institute Fellowship hosted at the University of Chicago and the Field Museum, I worked to constrain the molecular fingerprint of Life as we know it, based on computational, experimental, and analytical work. I am a passionate teacher, seasoned mentor (13 undergraduate-to-postdoctoral mentees), and a proud advocate for women in STEM and first-generational academics.

Teaching at Johns Hopkins University
I have taught more than 20 classes/courses/seminars/lectures/workshops on both the undergraduate and graduate student level prior to starting my position at JHU - in my classes, I cover traditional and frontier research concepts and methodologies across the sciences, connected through timely and interesting narratives. I believe that the most useful classes teach transferable methods and critical thinking: foundational skills that enable independent research!

Given that we work at the interface of geology, chemistry, and biology, and employ statistical methods for data analysis, I will be offering
classes that cover all aspects of our work in the coming fall term:

Deciphering the history of Life [AS.271.406 (01)] offered in the Morton K. Blaustein of Earth and Planetary Science at Johns Hopkins University.

Instructor: J. Wiemann. MW | 3 hours/week. Chemistry, Organismal & Evolutionary Biology, Statistics.

The Dynamic Earth: An Introduction to Geology [AS.270.220 (01)] offered in the Morton K. Blaustein of Earth and Planetary Science at Johns Hopkins University.

Instructors: D. Viete, J. Wiemann. TTh | 3 hours/week. Geology, Mineralogy.


The Dynamic Earth Laboratory [AS.270.221 (01)] offered in the Morton K. Blaustein of Earth and Planetary Science at Johns Hopkins University.

Instructors: D. Viete, J. Wiemann. W | 2 hours/week. Geology, Mineralogy.

Postdoctoral Scholars (joining 2025)

Updates coming soon! 

PhD Students (starting in the fall of 2024)


Liam Olden, MRes

Joining us from: Perth, Western Australia


Cross-disciplinary expertise: Geology & Paleontology

                                      Sedimentology, Stratigraphy, 

                                      Geochemistry, Fossilization

                                      Micro- & Astrobiology

                                      Global Change Biology

Research interests: Evolution of biomineralization in prokaryote & eukaryote systems                           applied to predict adaptability ranges on a changing planet

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Megan Miller, BSc

Joining us from: Cleveland, United States of America


Cross-disciplinary expertise: Molecular Biology & Chemistry

                                      Genomics, Development, 

                                      Microbiology, Evolution

                                      Geology & Paleontology

                                      Global Change Biology

Research interests: Environmental, ecological, & developmental drivers of   

                         physiological evolution across the reptile clade (incl. birds)

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Undergraduate Students

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Emily Pituch
Johns Hopkins University
Earth and Planetary Sciences
Molecular and Cellular Biology

Research interests: Astrobiology,
                         Prebiotic chemistry,

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Ana Sofia Cancio Trelfa
Johns Hopkins University
Earth and Planetary Sciences

Research interests: Vertebrate paleontology,
                         Invertebrate paleontology,

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Opportunities in the lab - Join us!