Coarsening in Coral Skeletons Formation
ORAL
Abstract
Spherulites in coral skeletons are composed of acicular aragonite crystals radiating from common centers and exhibiting a 0–35° misorientation of crystallographic c-axes across grain boundaries, previously misattributed entirely to a mechanism called non-crystallographic branching [1,2]. Here, we examine skeletons from 9 diverse species with quantitative nanoscale crystal orientation analyses using Polarization-dependent Imaging Contrast (PIC) mapping [3]. We discovered that, in addition to spherulites, 4 of the species also form tiny (0.2–2 µm), randomly oriented, equant crystals, termed sprinkles. Supported by theoretical phase field simulations, we propose that all initially nucleated crystals are randomly oriented sprinkles, and that these later coarsen, with radially oriented crystals growing at the expense of smaller, randomly oriented sprinkles. This mechanism is analogous to solidification or annealing in metals, both of which are high-temperature phenomena, whereas in coral skeletons coarsening occurs at ambient conditions.
1. Sun 2017, DOI: 10.1021/acsnano.7b00127
2. Gránásy 2005, DOI: 10.1103/PhysRevE.72.011605
3. Gilbert 2017, DOI: 10.1016/j.epsl.2016.11.012
1. Sun 2017, DOI: 10.1021/acsnano.7b00127
2. Gránásy 2005, DOI: 10.1103/PhysRevE.72.011605
3. Gilbert 2017, DOI: 10.1016/j.epsl.2016.11.012
*Supported by:
NSF 1603192
DOE: DE-FG02-07ER15899
DOE: DE-AC02-05CH11231
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Presenters
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Chang-Yu Sun
- Department of Physics, University of Wisconsin - Madison
- University of Wisconsin - Madison