Paleoclimate Scientist Udara Amarathunga on an International Ocean Discovery Program to the Gibraltar Strait
Dec. 28, 2023

FOR IMMEDIATE RELEASE: Today, the exchange of the waters between the Mediterranean Sea and the Atlantic Ocean collide through a single gateway in the Gibraltar Strait. Approximately eight million years ago there were two other gateways: one in northern Morocco and the other through southern Spain. These connections…

Bering Land Bridge formed surprisingly late during last ice age
Jan. 3, 2023
A new study shows that the Bering Land Bridge, the strip of land that once connected Asia to Alaska, emerged far later during the last ice age than previously thought. (Sigman, Farmer, Pico ’14 mention)
Exploration of open ocean seaweed cultivation selected for inaugural Dean for Research fund for the Sustainability of Our Planet award
Sept. 30, 2022
Written by Catherine Zandonella, Office of the Dean for Research

An exploratory project to investigate the benefits of farming seaweed in the open ocean has been selected for funding from Princeton’s Dean for Research Innovation Fund for the Sustainability of Our Planet.

Climate change and ocean oxygen: Oxygen-poor zones shrank under past warm periods, scientists discover
Aug. 31, 2022

In the last 50 years, oxygen-deficient zones in the open ocean have increased. Scientists have attributed this development to rising global temperatures: Less oxygen dissolves in warmer water, and the tropical ocean’s layers can become more stratified.

But now... (SigmanAuderset)

Shark Week was every week for megalodon
July 26, 2022

New Princeton research shows that prehistoric megatooth sharks, the biggest sharks that ever lived, were apex predators at the highest level ever measured. Featured video a YouTube video with Prof. Daniel Sigman and Emma Kast *20.

The Arctic Ocean’s deep past provides clues to its imminent future
Aug. 16, 2021
Written by Liz Fuller-Wright, Office of Communications

With shrinking sea ice, more light reaches the surface of the Arctic Ocean. Some have predicted that this will lead to more plankton, which in turn would support fish and other animals. Not so fast, says a team of scientists led by Princeton University and the Max Planck Institute for Chemistry. They point to nitrogen, a vital nutrient. The researchers used fossilized plankton to study the history of sources and supply rates of nitrogen to the western and central open Arctic Ocean. Their work, detailed in a paper in the current issue of the journal Nature Geoscience, suggests that under a global warming regime, these open Arctic waters will experience more intense nitrogen limitation, likely preventing a rise in productivity. “Looking at the Arctic Ocean from space, it’s difficult to see water at all, as much of the Arctic Ocean is covered by a layer of sea ice,” said lead author Jesse Farmer, a postdoctoral research associate in the Department of Geosciences at Princeton University who is also a visiting postdoctoral fellow at the Max Planck Institute for Chemistry in Mainz, Germany. This sea ice naturally expands during winters and contracts during summers. In recent decades, however, global warming has caused a rapid decline in summer sea ice coverage, with summer ice cover now roughly half that of 1979.

A Long Term Perspective on Climate Change - When Earth Was 20 Degrees Warmer and Crocodiles Roamed Antarctica
March 3, 2021
Written by Lynn Thoman, 3 Takeaways

Did you know that Antarctica used to be ice-free and earth used to be 20 degrees warmer than it is now? Find out why climate change then wasn’t a problem, and why it is now with Princeton University’s Daniel Sigman. Also find out how climate change caused horses to grow from the size of large house cats to their size today. (Audio only)

What caused the ice ages? Tiny ocean fossils offer key evidence
Dec. 10, 2020
Written by Liz Fuller-Wright, Office of Communications
Since the discovery that atmospheric carbon dioxide (CO2) concentrations were lower during past ice ages, the cause has been a mystery. "The cause of the ice ages is one of the great unsolved problems in the geosciences,” said Daniel Sigman, the Dusenbury Professor of Geological and Geophysical Sciences. “Explaining this dominant climate phenomenon will improve our ability to predict future climate change.” (Ai mention)
Ocean provides a buffer against climate change
Oct. 29, 2019
Written by Video Production Support and the Office of Communications
Professors Laure Resplandy and Daniel Sigman explain how the ocean absorbs heat and carbon dioxide, providing a buffer against climate change. Researchers are modeling the long-term impacts to marine ecosystems and climate. (Video by Video Production Support and the Office of Communications)
Emma Kast one of seven graduate students honored
April 30, 2019
Written by Denise Valenti, Office of Communications
Emma Kast, one of seven graduate students awarded by The Graduate School in its annual Teaching Awards in recognition of their outstanding abilities as teachers.
Princeton geoscientists find new fallout from ‘the collision that changed the world’
April 25, 2019
Written by Liz Fuller-Wright, Office of Communications
When the landmass that is now the Indian subcontinent slammed into Asia about 50 million years ago, the collision changed the configuration of the continents, the landscape, global climate and more. Now a team of Princeton University scientists has identified one more effect: the oxygen in the world’s oceans increased, altering the conditions for life. (Kast mention)
130-year-old brain coral reveals encouraging news for open ocean
Oct. 1, 2018
Written by Catherine Zandonella, Office of the Dean for Research
When nitrogen-based fertilizers flow into water bodies, the result can be deadly for marine life near shore, but what is the effect of nitrogen pollution far out in the open ocean? (Wang mention)
Carbon ‘leak’ may have warmed the planet for 11,000 years, encouraging human civilization
July 30, 2018
Written by Liz Fuller-Wright, Office of Communications
The oceans are the planet’s most important depository for atmospheric carbon dioxide on time scales of decades to millenia. But the process of locking away greenhouse gas is weakened by activity of the Southern Ocean, so an increase in its activity could explain the mysterious warmth of the past 11,000 years, an international team of researchers reports.
The future of carbon and heat uptake by the Southern Ocean
May 4, 2016
Written by High Meadows Environmental Institute (formerly PEI)

Heat uptake by the ocean is slowing the greenhouse gas-driven warming of the atmosphere, and the ocean represents the dominant long-term sink for the carbon dioxide gas deriving from fossil fuel use. However, these beneficial roles of the ocean are tempered by the slowness with which surface waters are carried into the deep ocean, through a process known as “deep ocean ventilation” that occurs at high latitudes. Moreover, most global climate models have predicted that deep ocean ventilation will slow further in the future as global warming proceeds. The Southern Ocean around Antarctica is active in deep ocean ventilation and thus particularly important in the uptake of fossil fuel carbon dioxide and global warming heat. Evidence will be presented that deep ocean ventilation by the Southern Ocean was slower during past ice ages and faster during warm interglacial periods. These findings raise the possibility that deep ocean ventilation by the Southern Ocean will accelerate into the global warming future, counter to most model-based expectations. The origins and significance of this apparent disagreement will be discussed.

Radio interview regarding iron fertilization during the last ice age
March 27, 2014
Written by CBC Vancouver Radio One

Prof. Daniel Sigman, co-author of the study "Iron Fertilization of the Sub-antarctic Ocean During the Last Ice Age" talks with Vancouver's CBC Radio One host Gregor Craigie on the scalability and viability of boosting salmon populations in coastal water off of British Columbia. (Audio only)

Dust in the wind drove iron fertilization during ice age
March 21, 2014
Written by Catherine Zandonella, Office of the Dean for Research
Researchers from Princeton University and the Swiss Federal Institute of Techonology in Zurich have confirmed that during the last ice age iron fertilization caused plankton to thrive in a region of the Southern Ocean.