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Daniel E. Morse

Researcher at University of California, Santa Barbara

Publications -  6
Citations -  3279

Daniel E. Morse is an academic researcher from University of California, Santa Barbara. The author has contributed to research in topics: Aragonite & Biomineralization. The author has an hindex of 6, co-authored 6 publications receiving 3154 citations.

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Molecular mechanistic origin of the toughness of natural adhesives, fibres and composites

TL;DR: In this article, the authors used the atomic force microscope to stretch the organic molecules exposed on the surface of freshly cleaved nacre and found that the elongation events occur for forces of a few hundred piconewtons, which are smaller than the forces of over a nanonewton required to break the polymer backbone in the threads.
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Control of crystal phase switching and orientation by soluble mollusc-shell proteins

TL;DR: In this paper, the authors showed that soluble polyanionic proteins alone are sufficient to control the crystal phase of calcite and calcite without the need for deposition of an intervening protein sheet.
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Does Abalone Nacre Form by Heteroepitaxial Nucleation or by Growth through Mineral Bridges

TL;DR: In this paper, the authors present experimental support for a model of abalone nacre growth that is based on mineral bridges between successive aragonite tablets rather than on heteroepitaxial nucleation.
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Molecular Cloning and Characterization of Lustrin A, a Matrix Protein from Shell and Pearl Nacre of Haliotis rufescens

TL;DR: The cDNA coding for Lustrin A, a newly described matrix protein from the nacreous layer of the shell and pearl produced by the abalone, Haliotis rufescens, a marine gastropod mollusc, is cloned and characterized.
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Critical Transitions in the Biofabrication of Abalone Shells and Flat Pearls

TL;DR: In this paper, X-ray diffraction and scanning electron microscopy analyses of the growth of these flat pearl composites reveal that biomineralization is initiated by the deposition of an organic sheet on the implanted substrate, followed by growth of a calcite layer with preferred {10.4}.