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Our Research

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Our research is focused on developing and utilising geochemical proxies to track environmental change in the oceans in time and space. Isotope and trace element records, extracted from the skeletons of marine calcifiers in particular (e.g. corals and  sclerosponges) that can inhabit shallow waters to deep-sea environments, are used to determine how climate and anthropogenic processes have influenced our oceans over recent and geological timescales. Integral to this work, is studying biomineralisation processes, and how they influence the geochemical compositions.

 

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Julie Trotter

Julie Trotter

ARC Future Fellow, Principal Research Fellow

+61 (0) 8 6488 3925

Here are some of the groups we are working with around the world

Instituto di Scienze Polari

 

 

 

Istituto di Scienze Marine

The University of Queensland

 

 

University of Puerto Rico

 

 

 

 

University of Indiana

 

 

 

 

Laboratoire des Sciences du Climat et de l’Environnement

 

 

 

 

 

University of Padova

 

 

 

 

Gechemical techniques commonly employed include boron isotopes and trace elements concentrations for reconstructing seawater pH, temperature, nutrient flux, carbonate ion and hence saturation state, in order to understand the processes of anthropogenic driven climate change and ocean acidification. The uranium-thorium disequilibrium dating technique is also used to analyse carbonates, which can provide absolute dates for samples ranging from >100,000 to several years in age. All geochemical preparation and mass spectrometry is undertaken in the state-of-the-art Advanced Geochemical Facility for Indian Ocean Research (see Facilities).

A range of biogenic archives underpin our research, which addresses present-day issues of climate change and ocean acidification, water pollution, as well as understanding environmental changes over longer (geological) timescales, that latter providing key boundary-conditions essential to constraining ocean-atmosphere models. Our research projects are utilising a range of species of shallow-water and increasingly deep-sea corals, and sclerosponges. Detailed characterisation of present-day conditions at the collection sites is used to ‘ground-truth’ the responses of these biogeochemical archives to climate and environmental changes.

 

The Oceans under Global Warming and Ocean Acidification

Shallow water coral reef environments are facing threats from both CO2 driven ocean warming as well as ocean acidification. State-of-the-art geochemical proxy studies of long-lived massive corals, sclerosponges, are used to track long-term changes in ocean temperature and carbonate chemistry (ie pH, carbonate ion) of waters from a range of environments, including shallow coral reef waters, the upper mixed layer inhabited by sclerosponges and increasingly the deep-sea-waters of the Southern Oceans. These studies aim to identify and characterise longer-term changes in the shallow as well as poorly known deep oceans. Our focus is increasingly on extreme events such as marine heatwaves but also the longer-term ability of the upper oceans to continue to sequester  greenhouse-generated heat and CO2  as well as the frequency and longer-term impacts accompanying these processes. Understanding the vulnerability of coral reef habitats that occur along Australia’s and especially Western Australia’s extensive coastline is of paramount interest.

Calcification and Biomineralisation in Changing Oceans

The ecology and geochemistry of a variety of marine calcifiers across the Western Australian coast (Kimberley, Exmouth, Abrolhos Islands, Perth, and Albany) are being studied to understand the influence of climate change on the calcification process. In-situ field studies are complemented by controlled experiments within laboratory flumes and mesocosms, in the purpose-built Watermans facility north of Perth (see Facilities).

Biomineralisation studies also utilise state-of-the-art facilities, such as Secondary ion mass spectrometry (SIMS) for high spatial resolution analyses; optical and electron microscopy; X-ray micro-computed tomography (micro-CT) and confocal Raman imaging and Atomic Force Microscope (AFM) located UWA’s Centre for Microscopy, Characterisation and Analysis (CMCA).

 

Pollution in Deep-Sea Canyons

 

 

Australia’s coastal zone contains some of the planets most spectacular and unique environments. Arguably the least well known are the deep-sea canyons that occur along the shelf edge of Australias continental margin.  The Perth Canyon is the largest of these systems and as its name suggests is located offshore  Perth the capital city of Western Australia.  Other canyons also occur offshore sw Western Australia in what were thought  to be more ‘pristine’ areas but are still subject to detectable levels of pollution from a surprising range of sources including commercial fishing as well defense related activities. As part of our international research program we are now documenting the character and prevalence of these various types of anthropogenic pollution in the deep-sea canyons as well as the nearby coastal waters  subject to a growing range of hazards from ever-increasing urbanisation and industrialisation.

 

Ocean-climate Change in Deep Water Environments

Geochemical proxy records extracted from deep-water coral skeletons are being used track environmental changes in intermediate to deep waters in space and time. A wide range of geochemical tools (including U-Th, 14C, εNd, δ13C, δ15N, Li/Mg, B/Ca, Ba/Ca, U/Ca) are being used to understand ocean-climate interactions at local and regional scales between the southeast Indian Ocean (Perth Canyon) and Antarctica. The aim is to characterise changes in ocean circulation patterns, climate trends, and carbon flux during recent (anthopogenic and pre-industrial) times and through the last glacial-interglacial cycle (~30-15 ka), in order to understand the drivers and long-term responses in Earth’s ocean-climate system during periods of major climate change.

 

 

 

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