Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)

Recent studies carried out in coral reef settings or under controlled conditions showed that rising aqueous pCO2 (pH ≥ 7.8 – 7.9, and a saturation state of carbonate minerals > 1) stimulates the growth of reef microboring or euendolithic phototrophs, especially microalgae, and therefore, enhance...

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Main Authors: Tribollet, Aline, Grange, Julie, Para, Hugo, Rodolfo-metalpa, Riccardo, Carreiro-silva, Marina
Format: Dataset
Language:unknown
Published: SEANOE 2017
Subjects:
Online Access:https://doi.org/10.17882/51167
id ftseanoe:oai:seanoe.org:51167
record_format openpolar
spelling ftseanoe:oai:seanoe.org:51167 2023-05-15T17:50:12+02:00 Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores) Tribollet, Aline Grange, Julie Para, Hugo Rodolfo-metalpa, Riccardo Carreiro-silva, Marina North 38.927723, South 38.206175, East -28.21509, West -29.225832 North 41.348655, South 40.150207, East 14.732277, West 12.974465 2017 https://doi.org/10.17882/51167 unknown SEANOE doi:10.17882/51167 http://dx.doi.org/10.17882/51167 CC-BY-NC-SA CC-BY-NC-SA carbonate dissolution microborers euendolithic flora CO2 vents ocean acidification biogenic dissolution temperate-cold coastal systems Ischia Island Faial Island bioerosion mollusk shells coral skeletons dataset 2017 ftseanoe https://doi.org/10.17882/51167 2021-12-09T18:22:38Z Recent studies carried out in coral reef settings or under controlled conditions showed that rising aqueous pCO2 (pH ≥ 7.8 – 7.9, and a saturation state of carbonate minerals > 1) stimulates the growth of reef microboring or euendolithic phototrophs, especially microalgae, and therefore, enhance rates of biogenic dissolution of carbonates. Those micro-organisms play a major role in reef bioerosion and coral reef functioning. In temperate-cold carbonate ecosystems, carbonate dissolution by euendolithic microflora has never been investigated under natural ocean acidification conditions. We thus realized two experiments to investigate the effects of low pH (and saturation states) on early natural microboring communities colonizing various carbonates and their associated rates of biogenic dissolution. One was carried out at Ischia (Italy) with mollusk shells exposed at two CO2 vents (pH < 7.5) vs an ambient site (pH ~ 8) during six months. The other one was realized at Faial (Azores) with various carbonate substrates (both aragonite and calcite) at one CO2 vent (pH ~ 7.4) vs an ambient site (pH ~ 8) over 45 days. Here we provide the data which allowed calculating rates of carbonate biogenic dissolution at all studied sites; i.e. the depth of penetration of euendolithic filaments into carbonates and the % of surface area of substrate colonized by microborers (bioeroded surface area). Rates of biogenic dissolution per site and per location are also provided, as well as environmental data collected at Faial (those collected at Ischia are published elsewhere). A total of 5 excel files is thus provided. Dataset Ocean acidification SEANOE (Sea scientific open data publication)
institution Open Polar
collection SEANOE (Sea scientific open data publication)
op_collection_id ftseanoe
language unknown
topic carbonate dissolution
microborers
euendolithic flora
CO2 vents
ocean acidification
biogenic dissolution
temperate-cold coastal systems
Ischia Island
Faial Island
bioerosion
mollusk shells
coral skeletons
spellingShingle carbonate dissolution
microborers
euendolithic flora
CO2 vents
ocean acidification
biogenic dissolution
temperate-cold coastal systems
Ischia Island
Faial Island
bioerosion
mollusk shells
coral skeletons
Tribollet, Aline
Grange, Julie
Para, Hugo
Rodolfo-metalpa, Riccardo
Carreiro-silva, Marina
Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)
topic_facet carbonate dissolution
microborers
euendolithic flora
CO2 vents
ocean acidification
biogenic dissolution
temperate-cold coastal systems
Ischia Island
Faial Island
bioerosion
mollusk shells
coral skeletons
description Recent studies carried out in coral reef settings or under controlled conditions showed that rising aqueous pCO2 (pH ≥ 7.8 – 7.9, and a saturation state of carbonate minerals > 1) stimulates the growth of reef microboring or euendolithic phototrophs, especially microalgae, and therefore, enhance rates of biogenic dissolution of carbonates. Those micro-organisms play a major role in reef bioerosion and coral reef functioning. In temperate-cold carbonate ecosystems, carbonate dissolution by euendolithic microflora has never been investigated under natural ocean acidification conditions. We thus realized two experiments to investigate the effects of low pH (and saturation states) on early natural microboring communities colonizing various carbonates and their associated rates of biogenic dissolution. One was carried out at Ischia (Italy) with mollusk shells exposed at two CO2 vents (pH < 7.5) vs an ambient site (pH ~ 8) during six months. The other one was realized at Faial (Azores) with various carbonate substrates (both aragonite and calcite) at one CO2 vent (pH ~ 7.4) vs an ambient site (pH ~ 8) over 45 days. Here we provide the data which allowed calculating rates of carbonate biogenic dissolution at all studied sites; i.e. the depth of penetration of euendolithic filaments into carbonates and the % of surface area of substrate colonized by microborers (bioeroded surface area). Rates of biogenic dissolution per site and per location are also provided, as well as environmental data collected at Faial (those collected at Ischia are published elsewhere). A total of 5 excel files is thus provided.
format Dataset
author Tribollet, Aline
Grange, Julie
Para, Hugo
Rodolfo-metalpa, Riccardo
Carreiro-silva, Marina
author_facet Tribollet, Aline
Grange, Julie
Para, Hugo
Rodolfo-metalpa, Riccardo
Carreiro-silva, Marina
author_sort Tribollet, Aline
title Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)
title_short Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)
title_full Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)
title_fullStr Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)
title_full_unstemmed Data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at Ischia (Italy) and Faial (Azores)
title_sort data related to biogenic dissolution rates quantified in various carbonate substrates exposed to ocean acidification at ischia (italy) and faial (azores)
publisher SEANOE
publishDate 2017
url https://doi.org/10.17882/51167
op_coverage North 38.927723, South 38.206175, East -28.21509, West -29.225832
North 41.348655, South 40.150207, East 14.732277, West 12.974465
genre Ocean acidification
genre_facet Ocean acidification
op_relation doi:10.17882/51167
http://dx.doi.org/10.17882/51167
op_rights CC-BY-NC-SA
op_rightsnorm CC-BY-NC-SA
op_doi https://doi.org/10.17882/51167
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