By using a non-invasive electron beam, SEM creates images of both high resolution and high magnification at the same time. These analyses provide detailed information about morphology, microstructure or elemental composition of samples.
For over 70 years, the Roman Kozłowski Institute of Paleobiology has been conducting in-depth studies of the history of life on Earth. Every year, the Institute publishes dozens of peer-reviewed articles, organizes conferences, foreign expeditions and excavations in new paleontological sites. We educate PhD students, publish the best paleontological journal in Poland (Acta Palaeontologica Polonica) and popularize science. The staff and laboratories are open to cooperation with other research centers and interdisciplinary projects. An essential part of our Institute is the Paleontological Collection, gathering the largest fossil collections in Poland (hundreds of thousands of specimens), partly exhibited in the Museum of Evolution.
The over-thousand-page monograph on the largest mountain range in Palaeozoic Europe—the Variscan orogen—also includes a chapter on brachiopods. These are among the most common Silurian, Devonian, and Carboniferous fossils in this area (at least 1,500 species), providing numerous elements for palaeoecological and palaeobiogeographic reconstructions.
Exceptionally well-preserved sub-fossil colonies of Cladocora sp. corals from the Hellenistic port of Acre (ca. 335–94 BCE) have made it possible to combine archaeological and modern data, providing a better understanding of climate variability and human influence on ancient coastal processes more than 2000 years ago.
Imagine a microscope so powerful it can “see” molecules a billion times more precisely than traditional tools. That’s what Photo-induced Force Microscopy (PiFM) does, offering new insights into Earth and environmental sciences.
New, very sensitive methods allowed analysing seasonal changes of strontium isotopes in woolly mammoth teeth, thus enabling analysis with under 10-day resolution over more than 10 years of tooth growth.
Throughout their long evolutionary history, crinoids developed pseudoplanktonic lifestyles and attached themselves with long stalks to driftwood. This article describes the microstructure and internal morphology of the stalks of such crinoids from the genus Seirocrinus.
Institute of Paleobiology has received financial support for research and educational projects from:
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