Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells
56 million years ago, the Earth underwent a rapid climate change event called the “Paleocene Eocene Thermal Maximum” (PETM). Sedimentary records show that a massive amount of carbon was released into the atmosphere, causing ocean acidification, warming, and a widespread extinction of deep-sea organi...
Main Author: | |
---|---|
Format: | Text |
Language: | unknown |
Published: |
Montclair State University Digital Commons
2019
|
Subjects: | |
Online Access: | https://digitalcommons.montclair.edu/sustainability-seminar/2019/fall2019/10 https://digitalcommons.montclair.edu/context/sustainability-seminar/article/1063/viewcontent/Haynes_Seminar_flier.pdf |
id |
ftmontclairstuni:oai:digitalcommons.montclair.edu:sustainability-seminar-1063 |
---|---|
record_format |
openpolar |
spelling |
ftmontclairstuni:oai:digitalcommons.montclair.edu:sustainability-seminar-1063 2023-07-23T04:21:05+02:00 Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells Haynes, Laura 2019-11-13T00:00:00Z application/pdf https://digitalcommons.montclair.edu/sustainability-seminar/2019/fall2019/10 https://digitalcommons.montclair.edu/context/sustainability-seminar/article/1063/viewcontent/Haynes_Seminar_flier.pdf unknown Montclair State University Digital Commons https://digitalcommons.montclair.edu/sustainability-seminar/2019/fall2019/10 https://digitalcommons.montclair.edu/context/sustainability-seminar/article/1063/viewcontent/Haynes_Seminar_flier.pdf Sustainability Seminar Series Earth Sciences Environmental Sciences text 2019 ftmontclairstuni 2023-07-03T21:43:50Z 56 million years ago, the Earth underwent a rapid climate change event called the “Paleocene Eocene Thermal Maximum” (PETM). Sedimentary records show that a massive amount of carbon was released into the atmosphere, causing ocean acidification, warming, and a widespread extinction of deep-sea organisms. Reconstructing the source and amount of carbon released during the PETM has been a major focus for paleoclimatologists as we seek to understand how the Earth system will respond to modern carbon emissions and warming. To help quantify ocean acidification at the PETM, we are using the boron content (the B/Ca ratio) of the shells of fossilized foraminifera as a proxy for past ocean pH and carbon content. I will present new calibrations for the B/Ca proxy that we have created by growing living planktic foraminifera in seawater chemistry analogous to that of the Paleogene and simulating severe ocean acidification. I will discuss the best way to apply these new calibrations from modern species to now-extinct Paleogene foraminifera and will show how our calibrations shed new light on the size and source of the PETM ocean acidification event. Text Ocean acidification Montclair State University Digital Commons |
institution |
Open Polar |
collection |
Montclair State University Digital Commons |
op_collection_id |
ftmontclairstuni |
language |
unknown |
topic |
Earth Sciences Environmental Sciences |
spellingShingle |
Earth Sciences Environmental Sciences Haynes, Laura Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells |
topic_facet |
Earth Sciences Environmental Sciences |
description |
56 million years ago, the Earth underwent a rapid climate change event called the “Paleocene Eocene Thermal Maximum” (PETM). Sedimentary records show that a massive amount of carbon was released into the atmosphere, causing ocean acidification, warming, and a widespread extinction of deep-sea organisms. Reconstructing the source and amount of carbon released during the PETM has been a major focus for paleoclimatologists as we seek to understand how the Earth system will respond to modern carbon emissions and warming. To help quantify ocean acidification at the PETM, we are using the boron content (the B/Ca ratio) of the shells of fossilized foraminifera as a proxy for past ocean pH and carbon content. I will present new calibrations for the B/Ca proxy that we have created by growing living planktic foraminifera in seawater chemistry analogous to that of the Paleogene and simulating severe ocean acidification. I will discuss the best way to apply these new calibrations from modern species to now-extinct Paleogene foraminifera and will show how our calibrations shed new light on the size and source of the PETM ocean acidification event. |
format |
Text |
author |
Haynes, Laura |
author_facet |
Haynes, Laura |
author_sort |
Haynes, Laura |
title |
Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells |
title_short |
Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells |
title_full |
Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells |
title_fullStr |
Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells |
title_full_unstemmed |
Quantifying ocean acidification in the geologic record using the B/Ca ratio of planktic foraminifera shells |
title_sort |
quantifying ocean acidification in the geologic record using the b/ca ratio of planktic foraminifera shells |
publisher |
Montclair State University Digital Commons |
publishDate |
2019 |
url |
https://digitalcommons.montclair.edu/sustainability-seminar/2019/fall2019/10 https://digitalcommons.montclair.edu/context/sustainability-seminar/article/1063/viewcontent/Haynes_Seminar_flier.pdf |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Sustainability Seminar Series |
op_relation |
https://digitalcommons.montclair.edu/sustainability-seminar/2019/fall2019/10 https://digitalcommons.montclair.edu/context/sustainability-seminar/article/1063/viewcontent/Haynes_Seminar_flier.pdf |
_version_ |
1772186271369658368 |