David H. Kohn 2026-11-05
David H. Kohn is a biomedical engineer whose research connects biomineralization, biomaterials and biomechanics. His University of Michigan profile describes two related questions: how the organization of mineralized tissue produces its mechanical behavior, and how understanding natural material formation can inform engineered biomaterials. This is an example of biomimetics: learning design principles from biological structures rather than merely copying their chemical ingredients.[ref]
David H. Kohn, from his University of Michigan faculty profile
. His joint work with M. D. Morris, W. F. Finney and Rupak M. Rajachar used Raman spectroscopy to investigate bone during elastic deformation. Their custom mechanical tester fitted the stage of a Raman microprobe and accepted hydrated specimens. The experiment paired loading of murine femora in tension with measurements of mineral phosphate-band shifts, while keeping loading below yield.[ref]
Bone tissue ultrastructural response to elastic deformation probed by Raman spectroscopy by Michael D. Morris and others. Abstract: mechanical tester, hydrated specimens and elastic-regime mineral response
The combination asks how a local molecular response accompanies the deformation of an entire composite material.An original idealized calculation explains why the two measurements are complementary. For a harmonic oscillator with effective bond force constant and reduced mass , the vibrational wavenumber iswhere is the speed of light. Holding fixed gives the first-order relation . A hypothetical band moving from to would correspond to approximately a decrease in this model's effective bond force constant. This Raman shift as a probe of bond stiffness is a local vibration model; the chosen numbers are not measurements from Kohn's paper.
A specimen's Young's modulus instead relates its macroscopic stress to its strain in a specified loading direction and regime. It cannot be read directly from one vibrational wavenumber. Composite material geometry, phase interactions and orientation mediate the connection between a local bond force constant and a bulk elastic modulus. Even a large local spectral response need not imply an equally large change in bulk stiffness.
This distinction gives the experiment its interest: a tensile testing apparatus and a spectroscopic probe observe different levels of the same loaded material. Their agreement or disagreement can discriminate structural explanations that a single bulk measurement would leave unresolved. Repeating both measurements during unloading would additionally test whether the changes reverse. Kohn's institutional description places this multiscale mechanics question alongside the development of new biomaterials.[ref]
David Kohn profile at the University of Michigan. Research Interests: tissue organization, mechanical competence and material design
Marie Albéric 2026-11-05
Marie Albéric is a researcher in biomineralization and the structure of biological materials. Her institutional publication record directly identifies the author credited as M. Albéric in the 2018 study of mineralized collagen organization in elephant ivory.[ref]
Marie Albéric publication record at the Max Planck Institute of Colloids and Interfaces. Named researcher record, 2018 Acta Biomaterialia publication
That study combined X-ray scattering, polarized light microscopy and scanning electron microscopy to investigate how the orientation of mineralized collagen varies across the tusk. It described distinct structural arrangements near the outside and within the middle region. The authors proposed that this organization, together with birefringence, contributes to the bright-and-dark Schreger pattern, while treating its detailed structural origin as a question requiring evidence.[ref]
The three-dimensional arrangement of the mineralized collagen fibers in elephant ivory and its relation to mechanical and optical properties by M. Albéric and others. Abstract, complementary methods, orientation gradients and optical interpretation
A constructed geometry example explains the need for multiple views. A straight fiber segment of length lies at angle to a chosen axis. Its components along that axis and a perpendicular axis are and . For and , these are approximately and . A two-dimensional view can shorten an obliquely oriented structure; projected length alone cannot reveal both true length and three-dimensional orientation.
Albéric and collaborators' contribution connects hierarchical structure with optical behavior rather than treating ivory as a uniform solid. Complementary measurements constrain different aspects of the model: an orientation-sensitive signal and a structural image need not report the same quantity, even when both concern the same collagen network.
N. Kröger 2026-11-05
N. Kröger investigated how diatoms build intricately patterned silica structures. A 1999 study isolated positively charged peptides, named silaffins, from diatom biosilica. Adding these molecules to a solution of silicic acid generated networks of silica nanospheres outside the living cell.[ref]
Reconstituting this step gave evidence that organic components can directly influence mineral formation. It did not require an intact diatom to make every sphere, while also not claiming that the isolated peptides alone reconstruct the whole shell. The experiment connects biomineralization to the properties of particular biological molecules.
A mass extinction is driven by changes that overwhelm organisms' physiological tolerances or destroy their food and habitat systems. Distinguish the initiating forcing from the linked environmental mechanisms: one event can generate several contributors.
- Large extraterrestrial impact. At the Cretaceous–Palaeogene boundary, the Chicxulub impact injected dust, aerosols and soot that reduced incoming sunlight and photosynthesis, disrupting food webs; rapid heating, fires and subsequent cooling added stresses. The impact is the trigger, while darkness and loss of primary production are proximate mechanisms.
- Large-scale volcanism. Eruption and intrusion of large igneous provinces, notably the Siberian Traps around the end-Permian crisis, release or mobilize gases and can produce rapid climate change. Carbon dioxide favors warming; sulfur-bearing emissions can cause shorter cooling and acid deposition. The outcome depends on rate, duration and interacting reservoirs, rather than eruption volume alone.
- Ocean anoxia and euxinia. Warming lowers oxygen solubility and can strengthen stratification; altered nutrient supply increases oxygen demand. Oxygen loss removes habitable marine volume, while sulfide in anoxic waters can be toxic. These processes contributed to the end-Permian marine crisis and can reinforce warming-driven mortality.
- Ocean ocean acidification and elevated carbon dioxide. Rapid addition of carbon dioxide changes seawater carbonate chemistry and can impair biomineralization, while high carbon dioxide also challenges physiological acid–base regulation. Susceptibility varies with physiology; this is a linked mechanism rather than proof that every calcifying group responds identically.
- Rapid cooling and eustatic sea level change. Late Ordovician glaciation and regression reduced shallow-marine habitat and changed temperatures and circulation; subsequent warming and oxygen loss introduced a different set of stresses. Habitat loss and climate change can therefore contribute in successive phases of one crisis.
These examples supply more than four drivers or contributors. The historical effects of volcanism, warming, oxygen loss and elevated carbon dioxide can act together rather than compete as mutually exclusive explanations.[ref]
Paleophysiology and end-Permian mass extinction by Andrew H. Knoll and others. Abstract and introduction: linked physiological effects of warming, anoxia, sulfide and hypercapnia

