Chemical and Biological Controls on Coral Nucleation

Thesis (Ph.D.)--University of Washington, 2021 Coral reefs are vibrant and important ecosystems in the oceans, but reefs today are under threat from multiple sources. One such threat is ocean acidification due to anthropogenic climate change, which is reducing both seawater pH and the thermodynamic...

Full description

Bibliographic Details
Main Author: Wolfshorndl, Marta Pinney
Other Authors: Gagnon, Alexander
Format: Thesis
Language:English
Published: 2021
Subjects:
Online Access:http://hdl.handle.net/1773/47116
id ftunivwashington:oai:digital.lib.washington.edu:1773/47116
record_format openpolar
spelling ftunivwashington:oai:digital.lib.washington.edu:1773/47116 2023-05-15T17:50:22+02:00 Chemical and Biological Controls on Coral Nucleation Wolfshorndl, Marta Pinney Gagnon, Alexander 2021 application/pdf http://hdl.handle.net/1773/47116 en_US eng supplemental_tables.xlsx; spreadsheet; Tables that were too large to fit in the thesis document. Wolfshorndl_washington_0250E_22522.pdf http://hdl.handle.net/1773/47116 CC BY biomineralization climate change corals nucleation ocean acidification organic matrix Geochemistry Chemical oceanography Oceanography Thesis 2021 ftunivwashington 2023-03-12T19:00:49Z Thesis (Ph.D.)--University of Washington, 2021 Coral reefs are vibrant and important ecosystems in the oceans, but reefs today are under threat from multiple sources. One such threat is ocean acidification due to anthropogenic climate change, which is reducing both seawater pH and the thermodynamic driving force for CaCO3-based biomineralization (oversaturation or ?). It is known that coral skeletal growth will decrease in an acidifying ocean, but the detailed mechanisms driving this response are still poorly understood. In addition, there is a long-standing debate in the field regarding the relative impact of skeletal organic matrix proteins on calcification and nucleation, with some claiming that these proteins can mitigate the effects of ocean acidification. Nucleation is the first step of the skeleton growing process, and as such is the step that is thought to determine the pace, pattern, and strength of the coral skeleton, and by extension, the development of the very framework that holds reefs together. We made the first quantitative measurements of inorganic aragonite nucleation and its sensitivity to ?, mapping the energy landscape of nucleation kinetics, and finding that it is more sensitive to oversaturation than bulk mineral growth rates in the environmentally relevant range of ? values. Furthermore, we combined inorganic mineral growth rates from the literature with the nucleation rates measured in this work in a numerical model to make predictions about how these two processes work together to affect the overall skeleton. In order to determine the extent of biological control over nucleation, we measured the quantitative effects of a peptide from the acidic domain of a matrix protein from Stylophora pistillata, as well as matrix protein analogues and polypeptides with different functional groups, on nucleation rates and other growth properties. We found that although the matrix protein and analogues had an effect on nucleation, it is unlikely that this protein can counteract the effects of ocean ... Thesis Ocean acidification University of Washington, Seattle: ResearchWorks
institution Open Polar
collection University of Washington, Seattle: ResearchWorks
op_collection_id ftunivwashington
language English
topic biomineralization
climate change
corals
nucleation
ocean acidification
organic matrix
Geochemistry
Chemical oceanography
Oceanography
spellingShingle biomineralization
climate change
corals
nucleation
ocean acidification
organic matrix
Geochemistry
Chemical oceanography
Oceanography
Wolfshorndl, Marta Pinney
Chemical and Biological Controls on Coral Nucleation
topic_facet biomineralization
climate change
corals
nucleation
ocean acidification
organic matrix
Geochemistry
Chemical oceanography
Oceanography
description Thesis (Ph.D.)--University of Washington, 2021 Coral reefs are vibrant and important ecosystems in the oceans, but reefs today are under threat from multiple sources. One such threat is ocean acidification due to anthropogenic climate change, which is reducing both seawater pH and the thermodynamic driving force for CaCO3-based biomineralization (oversaturation or ?). It is known that coral skeletal growth will decrease in an acidifying ocean, but the detailed mechanisms driving this response are still poorly understood. In addition, there is a long-standing debate in the field regarding the relative impact of skeletal organic matrix proteins on calcification and nucleation, with some claiming that these proteins can mitigate the effects of ocean acidification. Nucleation is the first step of the skeleton growing process, and as such is the step that is thought to determine the pace, pattern, and strength of the coral skeleton, and by extension, the development of the very framework that holds reefs together. We made the first quantitative measurements of inorganic aragonite nucleation and its sensitivity to ?, mapping the energy landscape of nucleation kinetics, and finding that it is more sensitive to oversaturation than bulk mineral growth rates in the environmentally relevant range of ? values. Furthermore, we combined inorganic mineral growth rates from the literature with the nucleation rates measured in this work in a numerical model to make predictions about how these two processes work together to affect the overall skeleton. In order to determine the extent of biological control over nucleation, we measured the quantitative effects of a peptide from the acidic domain of a matrix protein from Stylophora pistillata, as well as matrix protein analogues and polypeptides with different functional groups, on nucleation rates and other growth properties. We found that although the matrix protein and analogues had an effect on nucleation, it is unlikely that this protein can counteract the effects of ocean ...
author2 Gagnon, Alexander
format Thesis
author Wolfshorndl, Marta Pinney
author_facet Wolfshorndl, Marta Pinney
author_sort Wolfshorndl, Marta Pinney
title Chemical and Biological Controls on Coral Nucleation
title_short Chemical and Biological Controls on Coral Nucleation
title_full Chemical and Biological Controls on Coral Nucleation
title_fullStr Chemical and Biological Controls on Coral Nucleation
title_full_unstemmed Chemical and Biological Controls on Coral Nucleation
title_sort chemical and biological controls on coral nucleation
publishDate 2021
url http://hdl.handle.net/1773/47116
genre Ocean acidification
genre_facet Ocean acidification
op_relation supplemental_tables.xlsx; spreadsheet; Tables that were too large to fit in the thesis document.
Wolfshorndl_washington_0250E_22522.pdf
http://hdl.handle.net/1773/47116
op_rights CC BY
_version_ 1766157092347969536