Vote for your favorite mineral in #MinCup25! - Carpathite vs. Leucite
Brace for oddness in a match between one of the very few hydrocarbon minerals carpathite and the temperature-flipping mineral leucite.
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Rasbury, E. Troy, Hemming, N. Gary (2017) Boron Isotopes: A “Paleo-pH Meter” for Tracking Ancient Atmospheric CO2. Elements, 13 (4) 243-248 doi:10.2138/gselements.13.4.243

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleBoron Isotopes: A “Paleo-pH Meter” for Tracking Ancient Atmospheric CO2
JournalElements
AuthorsRasbury, E. TroyAuthor
Hemming, N. GaryAuthor
Year2017 (August 1)Volume13
Issue4
PublisherMineralogical Society of America
DOIdoi:10.2138/gselements.13.4.243Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID409209Long-form Identifiermindat:1:5:409209:8
GUID0
Full ReferenceRasbury, E. Troy, Hemming, N. Gary (2017) Boron Isotopes: A “Paleo-pH Meter” for Tracking Ancient Atmospheric CO2. Elements, 13 (4) 243-248 doi:10.2138/gselements.13.4.243
Plain TextRasbury, E. Troy, Hemming, N. Gary (2017) Boron Isotopes: A “Paleo-pH Meter” for Tracking Ancient Atmospheric CO2. Elements, 13 (4) 243-248 doi:10.2138/gselements.13.4.243
In(2017, August) Elements Vol. 13 (4) Mineralogical Society of America
Abstract/NotesThe boron isotope composition of calcium carbonate shells of marine organisms has the unique potential to record surface ocean pH, allowing the calculation of atmospheric pCO2 due to the established relationship between pH and the partial pressure of (atmospheric) CO2 (pCO2). This “paleo-pH meter” allows scientists to produce a record of the natural fluctuations of atmospheric pCO2 over geologic time, which will help us better understand the impacts of the recent anthropogenic addition of CO2 to Earth's atmosphere. Towards this end, a tremendous effort to understand the systematics of boron uptake in marine carbonates is underway. Here, we review the potential of boron isotopes to constrain ocean pH and, thus, atmospheric pCO2.


See Also

These are possibly similar items as determined by title/reference text matching only.

 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 6, 2025 06:48:09
Go to top of page