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.
Discovery Early Career Researcher Award - Grant ID: DE160100668
Funder
Australian Research Council
Funding Amount
$354,000.00
Summary
Are corals able to control their calcification in a changing ocean? The project aims to develop a new understanding of fundamental mechanisms responsible for coral calcification and its ability to acclimate to global warming and ocean acidification. Mineral skeleton formation by coral is the key process controlling the creation of reef structures upon which entire ecosystems depend. Despite the importance of coral to the function of reef ecosystems, how calcification works mechanistically within ....Are corals able to control their calcification in a changing ocean? The project aims to develop a new understanding of fundamental mechanisms responsible for coral calcification and its ability to acclimate to global warming and ocean acidification. Mineral skeleton formation by coral is the key process controlling the creation of reef structures upon which entire ecosystems depend. Despite the importance of coral to the function of reef ecosystems, how calcification works mechanistically within coral itself, and why small modifications of their physical and chemical habitat can have large effects on growth is presently poorly understood. This project seeks to provide this basic knowledge to improve our ability to assess the future of corals and help policy-makers take adequate measures to preserve coral reefs.Read moreRead less
Calcification and shell chemistry response of Southern Ocean planktic foraminifers to ocean acidification and changing climates. Plankton that form tiny calcium carbonate shells will be cultured to determine how they will respond to acidification of the Southern Ocean caused by rising CO2 in the atmosphere. The same experiments will be used to gauge from their fossil shells how the Southern Ocean has caused and responded to changing atmosphere CO2 over the last glacial climate cycle
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
A changing climate for calcification on the Great Barrier Reef: past, present and future. The Great Barrier Reef (GBR) is a national and international icon, recognised through its inscription as a World Heritage Area and economic and social value to Australians. Maintenance of the GBR as we know it is now compromised by a rapidly changing climate. Ocean acidification, warming water temperatures and increased freshwater will progressively be detrimental to the fundamental reef-building process ....A changing climate for calcification on the Great Barrier Reef: past, present and future. The Great Barrier Reef (GBR) is a national and international icon, recognised through its inscription as a World Heritage Area and economic and social value to Australians. Maintenance of the GBR as we know it is now compromised by a rapidly changing climate. Ocean acidification, warming water temperatures and increased freshwater will progressively be detrimental to the fundamental reef-building process of calcification. Informed policy and management strategies in a rapidly changing physical environment require determination, for short and long time frames, of the regional consequences and impacts of changing reef-building capacity.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.
Deciphering strategies polar phytoplankton employ to lessen iron limitation. The Southern Ocean is of global importance. It comprises one-third of the global ocean by area and disproportionately absorbs two-thirds of anthropogenic ocean heat and half of anthropogenic carbon dioxide (CO2) emissions even though phytoplankton in this region are chronically iron-limited. This project aims to understand why copper uptake by phytoplankton lessens the effects of iron limitation and how copper substitut ....Deciphering strategies polar phytoplankton employ to lessen iron limitation. The Southern Ocean is of global importance. It comprises one-third of the global ocean by area and disproportionately absorbs two-thirds of anthropogenic ocean heat and half of anthropogenic carbon dioxide (CO2) emissions even though phytoplankton in this region are chronically iron-limited. This project aims to understand why copper uptake by phytoplankton lessens the effects of iron limitation and how copper substitutes for iron. This knowledge is critical for evaluating the impacts and feedbacks between iron and copper in regulating Southern Ocean productivity and ultimately its ability to drawdown atmospheric CO2. The results from this project will facilitate the development of improved ecosystem models and conservation tools.Read moreRead less
Bubble, Bubble CO2 is the trouble: A Natural Ocean Acidification Experiment in a coral reef setting. Carbon dioxide seep sites expose shallow coral reefs in Papua New Guinea to volcanic carbon dioxide resulting in gradients of seawater ranging from pH 8.0 (normal) to a more acidic pH of 7.5. Some areas of these reefs experience carbon dioxide exposure equivalent to IPCC predictions for 2050 and 2100. This project will reconstruct seawater pH using radiocarbon as a novel tracer of carbon dioxide ....Bubble, Bubble CO2 is the trouble: A Natural Ocean Acidification Experiment in a coral reef setting. Carbon dioxide seep sites expose shallow coral reefs in Papua New Guinea to volcanic carbon dioxide resulting in gradients of seawater ranging from pH 8.0 (normal) to a more acidic pH of 7.5. Some areas of these reefs experience carbon dioxide exposure equivalent to IPCC predictions for 2050 and 2100. This project will reconstruct seawater pH using radiocarbon as a novel tracer of carbon dioxide input at a coral reef site that has been exposed to high carbon dioxide due to volcanic seeps (seep carbon dioxide has no carbon-14) for an unknown period of time (at least many decades, but possibly centuries). These results will help to understand the time it takes to change calcifying organisms into “winners” or “losers” as an analog for Ocean Acidification due to increased atmospheric carbon dioxide input.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