BH
Baerbel Hoenisch
Lamont-Doherty Earth Observatory of Columbia University
AGU Abstracts
Arctic Ocean pH history of the past 140,000 years based on δ11B in planktic foraminifera and microbial biomarkers in sediment records
PAST CLIMATE CHANGE IN EARTH'S POLAR REGIONS: LESSONS FOR THE FUTURE III ORAL
paleoceanography and paleoclimatology | 16 december 2022
Jannik Martens, Sarah Hurley, Helen K. Coxall, Mat...
The cold Arctic Ocean allows CO2 to dissolve more readily than in other regions, leading to accelerated ocean acidification (OA) with profound environ...
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Investigating shell thickness and preservation in two species of planktic foraminifera over millions of years
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY: GENERAL CONTRIBUTIONS I POSTER
paleoceanography and paleoclimatology | 13 december 2021
Olivia M. Gadson, Lloyd B. Anderson, Natalie Umlin...
Planktic foraminifera are abundant microorganisms in the oceans' sediment record. Their fossil shells reflect the chemistry of their environment from ...
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The Future of Storing, Provisioning and Using Paleo CO₂ Data
CENTENNIAL SESSION: THE 100S OF CO<SUB>2</SUB> II POSTERS
paleoceanography and paleoclimatology | 12 december 2019
Ross Whiteford, Baerbel Hoenisch, Vicki L. Ferrini...
Paleo CO2 data have traditionally been stored in a variety of formats with hundreds of measurements spread across multiple repositories. This makes it...
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