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
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
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.
Novel technologies to resolve the role of organic matter on iron chemistry and bioavailability in the South Pacific Ocean. This project promotes cross-disciplinary scientific collaborations at national and international levels to understand the role iron plays in regulating oceanic biodiversity, primary production and ability to mitigate climate change. This project will thus benefit to human society as a whole. New promising technologies will be developed to assess iron oceanic limitation, the ....Novel technologies to resolve the role of organic matter on iron chemistry and bioavailability in the South Pacific Ocean. This project promotes cross-disciplinary scientific collaborations at national and international levels to understand the role iron plays in regulating oceanic biodiversity, primary production and ability to mitigate climate change. This project will thus benefit to human society as a whole. New promising technologies will be developed to assess iron oceanic limitation, therefore fostering the international competitiveness of Australian research. This project will contribute to National Research Priority: Sustainable use of Australia's biodiversity. In addition, the proposed research is a vital element of global effort to advance our understanding of iron-related oceanic processes, as manifest in several international scientific programs.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE120100030
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
The role of Antarctic sea ice as a natural ocean fertiliser. This project will assess the importance of sea ice as a natural fertiliser in the climatically important polar region. The knowledge gained will aid climate modellers and Governmental policy-makers concerned with the commercial use of ocean iron fertilisation as an attempt to reduce human-induced atmospheric carbon dioxide and gain carbon credits.
Ocean fertilisation: a positive effect from Antarctica’s great thaw? This project will evaluate how the Antarctica's great thaw may fertilise the Southern Ocean with iron and help mitigate carbon dioxide emissions now and in the future. The Southern Ocean is anaemic, meaning that the iron levels are too low to sustain photosynthesis, a pathway by which the oceans transform carbon dioxide into carbon-rich sediments. There is evidence that melting ice may supply substantial amount of iron, capable ....Ocean fertilisation: a positive effect from Antarctica’s great thaw? This project will evaluate how the Antarctica's great thaw may fertilise the Southern Ocean with iron and help mitigate carbon dioxide emissions now and in the future. The Southern Ocean is anaemic, meaning that the iron levels are too low to sustain photosynthesis, a pathway by which the oceans transform carbon dioxide into carbon-rich sediments. There is evidence that melting ice may supply substantial amount of iron, capable of boosting marine life and removing carbon dioxide. As polar regions show the earliest and most severe impacts of anthropogenic activity, studying ice-ocean interactions is central to supporting national and international policy development that can effectively limit the worst impacts of climate change globally. Read moreRead less
Holding coral reefs together with soluble cement. This project aims to characterise and understand cement formation in coral reefs. Coral reefs are constructed by cementing together aragonite building blocks made by corals. The main cementing agent is high-magnesium calcite, the most soluble carbonate mineral and susceptible to ocean acidification. High-magnesium calcite cements are best developed on the high energy margins of coral reefs. This project will quantify how crustose coralline algae ....Holding coral reefs together with soluble cement. This project aims to characterise and understand cement formation in coral reefs. Coral reefs are constructed by cementing together aragonite building blocks made by corals. The main cementing agent is high-magnesium calcite, the most soluble carbonate mineral and susceptible to ocean acidification. High-magnesium calcite cements are best developed on the high energy margins of coral reefs. This project will quantify how crustose coralline algae produces high-magnesium calcite and controls the dissolution and reprecipitation of high-magnesium cements. This project intends to quantify rates of reef cementation, susceptibility to ocean acidification and warming, and possible mitigating effects of alkalinity addition.Read moreRead less
Hot iron: Are submarine volcanoes important for Southern Ocean iron supply? The scarcity of iron limits biological productivity and carbon uptake in the nutrient rich waters of the Southern Ocean. This project will explore for the first time the role of undersea "hot spot" volcanoes in supplying iron to surface waters, thus linking the solid earth and the biosphere. The project will measure iron abundance, reactivity and nutritional value in buoyant plumes emanating from vents near Heard/McDonal ....Hot iron: Are submarine volcanoes important for Southern Ocean iron supply? The scarcity of iron limits biological productivity and carbon uptake in the nutrient rich waters of the Southern Ocean. This project will explore for the first time the role of undersea "hot spot" volcanoes in supplying iron to surface waters, thus linking the solid earth and the biosphere. The project will measure iron abundance, reactivity and nutritional value in buoyant plumes emanating from vents near Heard/McDonald Islands, Australia's only active volcanoes. The project aims to estimate the hydrothermal contribution to regional biological productivity and extrapolate to the whole Southern Ocean. Successful outcomes will benefit Australia by identifying iron sources that govern productivity and carbon uptake of an economically important ecosystem.Read moreRead less
Indian Ocean Climate Change: Ningaloo Reef, a litmus test for the survival of coral reefs. Coral reefs are at the frontline from the effects of rapidly rising levels of carbon dioxide that is causing both global warming and oceans to become more acid-like. Our research program will determine how the survival of one of the World’s most pristine and best preserved coral reefs, Ningaloo Reef, is linked to the response of Australia’s Indian Ocean to climate change. For the first time, we will simula ....Indian Ocean Climate Change: Ningaloo Reef, a litmus test for the survival of coral reefs. Coral reefs are at the frontline from the effects of rapidly rising levels of carbon dioxide that is causing both global warming and oceans to become more acid-like. Our research program will determine how the survival of one of the World’s most pristine and best preserved coral reefs, Ningaloo Reef, is linked to the response of Australia’s Indian Ocean to climate change. For the first time, we will simulate realistic ‘future’ conditions and see how actual coral reef systems respond. This will provide a ‘yardstick’ against which the best-case survival potential of the world’s coral reefs can be assessed, critical for underpinning the urgently needed action to reduce greenhouse gas emissions if we are to ensure the survival of coral reefs.Read moreRead less