Element ratio (Sr/Ca, Ba/Ca, B/Ca, and Mg/Ca) profiles throughout the larval life stage of Mytilus edulis, 2011

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Autores principales: Dawber, Caroline F, Branson, O, Elderfield, Henry, Harper, Elizabeth M, Greaves, Mervyn, Gazeau, Frédéric, Gattuso, Jean-Pierre, Middelburg, Jack J
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2011
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author Dawber, Caroline F
Branson, O
Elderfield, Henry
Harper, Elizabeth M
Greaves, Mervyn
Gazeau, Frédéric
Gattuso, Jean-Pierre
Middelburg, Jack J
author_facet Dawber, Caroline F
Branson, O
Elderfield, Henry
Harper, Elizabeth M
Greaves, Mervyn
Gazeau, Frédéric
Gattuso, Jean-Pierre
Middelburg, Jack J
collection Datos científicos de ciencias marinas y ambientales
contents Rising anthropogenic CO2 in the surface ocean has raised serious concerns for the ability of calcifying organisms to secrete their shells and skeletons. Previous mollusc carbonate perturbation experiments report deleterious effects at lowered pH (7.8-7.4 pH units), including reduced shell length and thickness and deformed shell morphology. It is not clear whether the reduced shell growth results from a decrease in calcification rate due to lowered aragonite saturation or from an indirect effect on mollusc metabolism. We take a novel approach to discerning between these two processes by examining the impact of lowered pH on the 'vital-effect' associated with element ratios. Reported herein are the first element ratio (Sr/Ca, Ba/Ca, B/Ca, Mg/Ca and Mn/Ca) profiles throughout the larval life stage of Mytilus edulis. Element ratio data for individuals reared in ambient conditions provide new insights into biomineralization during larval development. Sr/Ca ratios are consistent with Sr incorporation in the mineral phase. Mg and Mn are likely hosted in an organic phase. The Ba partition coefficient of early larval shells is one of the highest reported in biogenic aragonite. The reason for the high Ba concentrations is unknown, but may reflect the assimilation of Ba from food and/or Ba concentration in an organic or amorphous carbonate phase. There is no observable difference in the way the studied elements are incorporated into the shells of individuals reared in ambient and lowered pH conditions. The reduced growth rate at lower pH may be a consequence of a disruption to the larval mollusc metabolism.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_769719
institution PANGAEA
language en
publishDate 2011
publisher PANGAEA
record_format pangaea
spellingShingle Element ratio (Sr/Ca, Ba/Ca, B/Ca, and Mg/Ca) profiles throughout the larval life stage of Mytilus edulis, 2011
Dawber, Caroline F
Branson, O
Elderfield, Henry
Harper, Elizabeth M
Greaves, Mervyn
Gazeau, Frédéric
Gattuso, Jean-Pierre
Middelburg, Jack J
Barium/Calcium ratio; Boron/Calcium ratio; Calcium; EPOCA; European Project on Ocean Acidification; ICP-Q-MS; Inductively coupled plasma-quadrupole-mass spectrometry; Magnesium/Calcium ratio; Mytilus edulis, shell mass; Sample ID; Species; Strontium/Calcium ratio
Rising anthropogenic CO2 in the surface ocean has raised serious concerns for the ability of calcifying organisms to secrete their shells and skeletons. Previous mollusc carbonate perturbation experiments report deleterious effects at lowered pH (7.8-7.4 pH units), including reduced shell length and thickness and deformed shell morphology. It is not clear whether the reduced shell growth results from a decrease in calcification rate due to lowered aragonite saturation or from an indirect effect on mollusc metabolism. We take a novel approach to discerning between these two processes by examining the impact of lowered pH on the 'vital-effect' associated with element ratios. Reported herein are the first element ratio (Sr/Ca, Ba/Ca, B/Ca, Mg/Ca and Mn/Ca) profiles throughout the larval life stage of Mytilus edulis. Element ratio data for individuals reared in ambient conditions provide new insights into biomineralization during larval development. Sr/Ca ratios are consistent with Sr incorporation in the mineral phase. Mg and Mn are likely hosted in an organic phase. The Ba partition coefficient of early larval shells is one of the highest reported in biogenic aragonite. The reason for the high Ba concentrations is unknown, but may reflect the assimilation of Ba from food and/or Ba concentration in an organic or amorphous carbonate phase. There is no observable difference in the way the studied elements are incorporated into the shells of individuals reared in ambient and lowered pH conditions. The reduced growth rate at lower pH may be a consequence of a disruption to the larval mollusc metabolism.
title Element ratio (Sr/Ca, Ba/Ca, B/Ca, and Mg/Ca) profiles throughout the larval life stage of Mytilus edulis, 2011
topic Barium/Calcium ratio; Boron/Calcium ratio; Calcium; EPOCA; European Project on Ocean Acidification; ICP-Q-MS; Inductively coupled plasma-quadrupole-mass spectrometry; Magnesium/Calcium ratio; Mytilus edulis, shell mass; Sample ID; Species; Strontium/Calcium ratio
url https://doi.org/10.1594/PANGAEA.769719