Southern Ocean oxygen variability since the last glacial maximum. Recently observed decreases in ocean oxygen concentration could decrease ocean biodiversity and accelerate climate change. This project will determine the links between climate change and ocean oxygenation since the last ice age, and provide a way to predict future oxygen concentrations.
DEEP SEA CORALS AS HIGH RESOLUTION RECORDERS OF SOUTHERN OCEAN NUTRIENT CHEMISTRY AND CIRCULATION. There is compelling evidence that the Earth has been warming dramatically since the end of the 19th century as a consequence of increasing atmospheric CO2. This study aims to understand the long-term role of the Southern Ocean as a 'store-house' for CO2, and its significance in controlling changes in the Earth's climate. We will use coral skeletons from the deep oceans as archives of ocean circu ....DEEP SEA CORALS AS HIGH RESOLUTION RECORDERS OF SOUTHERN OCEAN NUTRIENT CHEMISTRY AND CIRCULATION. There is compelling evidence that the Earth has been warming dramatically since the end of the 19th century as a consequence of increasing atmospheric CO2. This study aims to understand the long-term role of the Southern Ocean as a 'store-house' for CO2, and its significance in controlling changes in the Earth's climate. We will use coral skeletons from the deep oceans as archives of ocean circulation and nutrient levels. This information will help unravel how biological activity in the Southern Ocean has responded during previous episodes of climate change, and how this has controlled the levels of CO2 in the Earth's atmosphere. This will provide a better understanding of greenhouse warming and its effect on our future climate.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE150100107
Funder
Australian Research Council
Funding Amount
$369,536.00
Summary
What is the impact of abrupt climate change on the global carbon cycle? In the past 50 000 years there were several episodes of abrupt climate change during which atmospheric carbon dioxide rose significantly. This project aims to determine the causes of past abrupt changes in atmospheric carbon dioxide. The project is significant because understanding changes in the global carbon cycle is essential to estimate future climate trajectories. Innovatively, it will highlight the relationship between ....What is the impact of abrupt climate change on the global carbon cycle? In the past 50 000 years there were several episodes of abrupt climate change during which atmospheric carbon dioxide rose significantly. This project aims to determine the causes of past abrupt changes in atmospheric carbon dioxide. The project is significant because understanding changes in the global carbon cycle is essential to estimate future climate trajectories. Innovatively, it will highlight the relationship between Southern Hemisphere water masses and the marine carbon cycle during abrupt climate change. The expected outcomes include a better understanding of the interplay between Southern Ocean processes and the carbon cycle.Read moreRead less
Examining the vulnerability of ocean carbon biogeochemistry in a high CO2 world. Rising CO2 levels in the atmosphere from human activity is changing the biogeochemistry of the ocean, with large potential consequences on future atmospheric CO2. This work will explore these changes and will result in a more complete understanding of how the ocean will either accelerate or delay the increase in atmospheric CO2.
An Investigation into Oceanic CO2 Variability and its Influence on Atmospheric CO2 Concentrations. Carbon dioxide is a powerful greenhouse gas whose observed atmospheric increase is the central cause
of climate change. The associated environmental, social and economic impacts to Australia could be
staggering via coral reef degradation, loss of agricultural production, coastal erosion and extreme climate
events. This work aims to better our understanding of how the oceans may mediate the effec ....An Investigation into Oceanic CO2 Variability and its Influence on Atmospheric CO2 Concentrations. Carbon dioxide is a powerful greenhouse gas whose observed atmospheric increase is the central cause
of climate change. The associated environmental, social and economic impacts to Australia could be
staggering via coral reef degradation, loss of agricultural production, coastal erosion and extreme climate
events. This work aims to better our understanding of how the oceans may mediate the effects of climate
change for Australia and therefore has a strong national benefit. Quantifying the importance Australia's
oceanic CO2 sink will be important for Australian policy makers within international climate negotiations
and also for better management practices to ensure the future prosperity of Australia's coral reef
ecosystem.Read moreRead less
Are subterranean estuaries a source or sink of greenhouse gases? The aim of this project is to investigate the role of subterranean estuaries and submarine groundwater discharge on the marine cycle of the greenhouse gases carbon dioxide, methane, and nitrous oxide. The expected outcome of this project is a better understanding of the role of coastal environments as a net source or sink of greenhouse gases.
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE140100083
Funder
Australian Research Council
Funding Amount
$155,000.00
Summary
A gamma spectrometry facility for cutting edge environmental geochemistry investigations. A gamma spectrometry facility for cutting edge environmental geochemistry investigations: This project will provide a cutting edge gamma spectrometry facility. The facility will perform high precision radionuclide measurements to resolve complex environmental processes such as sediment accumulation, soil erosion, submarine groundwater discharge, atmospheric deposition, marine carbon scavenging, and water ma ....A gamma spectrometry facility for cutting edge environmental geochemistry investigations. A gamma spectrometry facility for cutting edge environmental geochemistry investigations: This project will provide a cutting edge gamma spectrometry facility. The facility will perform high precision radionuclide measurements to resolve complex environmental processes such as sediment accumulation, soil erosion, submarine groundwater discharge, atmospheric deposition, marine carbon scavenging, and water mass circulation. This project is significant because the data obtained will fill fundamental gaps in the understanding of carbon, nitrogen, and trace metal cycling in soils, groundwater, rivers, estuaries, and the ocean. The outcome of this project is a better understanding of regional and global biogeochemical cycles. Read moreRead less
Probing the response of Southern Ocean phytoplankton to changes in iron biogeochemistry, light and pH associated with climate change. Determining factors that influence the health and vitality of coastal and open-ocean regions is crucial to maintaining marine biodiversity and the Earth’s climatic balance. This research project will determine the role climate change and ocean acidification will have on the ability of Southern Ocean phytoplankton to flourish.
Deep-sea carbonate cycles and their role in glacial-interglacial atmospheric CO2 changes. The causes for past atmospheric carbon dioxide (CO2) changes and their mechanistic links to the histories of climate and ocean carbonate chemistry remain elusive, but may hold future-relevant information. This project aims to use novel methods to quantify deep ocean carbonate ion concentrations, a critical but poorly constrained parameter of the global carbon cycle, at 10 key locations spanning the global o ....Deep-sea carbonate cycles and their role in glacial-interglacial atmospheric CO2 changes. The causes for past atmospheric carbon dioxide (CO2) changes and their mechanistic links to the histories of climate and ocean carbonate chemistry remain elusive, but may hold future-relevant information. This project aims to use novel methods to quantify deep ocean carbonate ion concentrations, a critical but poorly constrained parameter of the global carbon cycle, at 10 key locations spanning the global ocean during the last 350 000 years. By feeding new data into a model, this project aims to gain critical insights into mechanisms controlling past deep-sea carbonate cycles and atmospheric CO2 changes, thereby leading to improved understandings of the climate system.Read moreRead less
Past to future changes in ocean dynamics and biogeochemistry. This project aims to understand the impact of changes in ocean circulation on marine biogeochemistry, climate and ultimately the Antarctic ice-sheet by combining transient simulations of the last glacial cycle performed with an Earth system model incorporating the compilation of paleoproxy records. The oceanic circulation has varied over the last glacial cycle (~140,000 years) and is expected to change over the coming centuries due t ....Past to future changes in ocean dynamics and biogeochemistry. This project aims to understand the impact of changes in ocean circulation on marine biogeochemistry, climate and ultimately the Antarctic ice-sheet by combining transient simulations of the last glacial cycle performed with an Earth system model incorporating the compilation of paleoproxy records. The oceanic circulation has varied over the last glacial cycle (~140,000 years) and is expected to change over the coming centuries due to rising atmospheric carbon dioxide. The project will measure future changes in oceanic circulation on ocean acidification and oxygen content with a state-of-the-art high-resolution ocean carbon cycle model. This will lead to improved understanding of processes and feedbacks within the Earth system.Read moreRead less