Boron Proxies in Paleoceanography and Paleoclimatology
Barbel Hoenisch, Stephen M. Eggins, Laura L. Haynes, Katherine A. Allen, Katherine D. Holland, Katja Lorbacher
John Wiley & Sons, Apr 22, 2019 - Science - 264 pages
Anthropogenic carbon dioxide emissions do not only warm our planet but also acidify our oceans. It is currently unclear to which degree Earth’s climate and marine life will be impacted by these changes but information from Earth history, particularly the geochemical signals of past environmental changes stored in the fossil remains of marine organisms, can help us predict possible future changes. This book aims to be a primer for scientists who seek to apply boron proxies in marine carbonates to estimate past seawater carbonate chemistry and atmospheric pCO2.
Boron proxies (δ11B and B/Ca) were introduced nearly three decades ago, with subsequent strides being made in understanding their mechanistic functioning. This text reviews current knowledge about the aqueous systematics, the inorganic and biological controls on boron isotope fractionation and incorporation into marine carbonates, as well as the analytical techniques for measurement of boron proxies. Laboratory and field calibrations of the boron proxies are summarized, and similarities between modern calibrations are explored to suggest estimates for proxy sensitivities in marine calcifiers that are now extinct. Example applications illustrate the potential for reconstructing paleo-atmospheric pCO2 from boron isotopes. Also explored are the sensitivity of paleo-ocean acidity and pCO2 reconstructions to boron isotope proxy systematics that are currently less well understood, including the elemental and boron isotopic composition of seawater through time, seawater alkalinity, temperature and salinity, and their collective impact on the uncertainty of paleo-reconstructions.
The B/Ca proxy is based on the same mechanistic principles as the boron isotope proxy, but empirical calibrations suggest seawater pH is not the only controlling factor. B/Ca therefore has the potential to provide a second carbonate parameter that could be paired with δ11B to fully constrain the ocean carbonate system, but the associated uncertainties are large. This text reviews and examines what is currently known about the B/Ca proxy systematics. As more scientists embark on characterizing past ocean acidity and atmospheric pCO2, Boron in Paleoceanography and Paleoclimatology provides a resource to introduce geoscientists to the opportunities and complications of boron proxies, including potential avenues to further refine them.
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alkalinity analysis aqueous aragonite B(OH B/Ca B/Ca ratios benthic foraminifers biogenic borate boric acid boron concentration boron isotope boron isotope fractionation boron isotopic composition boron proxy bulloides Ca2+ CaCO CaCO3 calcite calcium carbonate calculated carbonate chemistry Cenozoic constant coretop Cosmochimica Acta deep‐sea dissolution Earth and Planetary Elderfield Eocene experimental experiments Figure foraminifer species foraminifera Foster Geochimica et Cosmochimica Globigerinoides Henehan higher Hönisch and Hemming ICP‐MS incorporation inorganic Kaczmarek Klochko laboratory Lemarchand lobifera marine carbonates Marine Micropaleontology Martínez‐Botí mass spectrometry MC‐ICP‐MS measured Miocene N‐TIMS observed ocean acidification ocean pH paleo‐pH Paleoceanography pCO2 photosynthesis Planetary Science Planetary Science Letters planktic foraminifers planktonic Pleistocene precipitation rate predicted Raitzsch range reconstructions Rollion‐Bard ruber sacculifer salinity samples Sanyal seawater seawater pH sediments sensitivity slope solution spray chamber studies surface ocean symbiont‐barren symbiont‐bearing techniques tion Tripati Uchikawa uncertainty values variability variations wuellerstorfi Zeebe