Different Growth Modes Of Coral Skeletons Revealed By Crystal Orientation Map
ORAL
Abstract
Coral skeletons were assumed based on morphology to grow spherulitically, that is, as radially distributed acicular aragonite (CaCO3) crystals, with their c-axes radiating from points. Recently we showed with Polarization-dependent Imaging Contrast (PIC) maps [1,2] that Stylophora pistillata (Sp) coral skeleton indeed grow spherulitically [3,4]. Is this true for other species? We tested Balanophyllia europaea (Be) and found that Be and Sp differ: Sp has only spherulites, whereas Be has spherulites and randomly oriented equant crystals, we named “sprinkles”. We show here that sprinkles grow slowly, and spherulites grow rapidly, but both grow by particle attachment [6], and are faster than ion-by-ion aragonite growth. We propose that a new class of proteins exists, which we named crystal Growth Rate Influencing Proteins (GRIPs), based on the observation in PIC maps that they make crystals grow faster or slower.
1. PUPA Gilbert et al. PNAS 108, 11350, 2011
2. PUPA Gilbert et al. EPSL 460, 281, 2017
3. C-Y Sun et al. ACS Nano 11, 6612, 2017
4. T Mass et al. PNAS 114, E7670, 2017
5. L Pasquini et al. J R Soc Interface 12, 20150168, 2015
6. De Yoreo et al. Science 349, aaa6760, 2015
1. PUPA Gilbert et al. PNAS 108, 11350, 2011
2. PUPA Gilbert et al. EPSL 460, 281, 2017
3. C-Y Sun et al. ACS Nano 11, 6612, 2017
4. T Mass et al. PNAS 114, E7670, 2017
5. L Pasquini et al. J R Soc Interface 12, 20150168, 2015
6. De Yoreo et al. Science 349, aaa6760, 2015
*Supported by DOE grant DE-FG02-07ER15899 and NSF grant DMR-1603192
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Presenters
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Chang-Yu Sun
- Department of Physics, University of Wisconsin-Madison
- Department of Physics, University of Wisconsin–Madison
- Physics, Chemistry, Geoscience, Univ of Wisconsin
- University of Wisconsin-Madison