A/Prof Adriana Dutkiewicz

Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climates

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The exchange of carbon between oceanic plates, the deep Earth, and the atmosphere plays a significant role in modulating global climate1,2. Icehouse-greenhouse climate fluctuations have been attributed to changes in palaeogeography and solid Earth degassing3, particularly along continental arcs2,4,5, to arc weathering5 and to the sequestration of carbon into oceanic carbonate-rich sediments6. However, the proportions … Read more…

The way Earth’s surface moves has a bigger impact on shifting the climate than we knew

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Our planet has experienced dramatic climate shifts throughout its history, oscillating between freezing “icehouse” periods and warm “greenhouse” states. Scientists have long linked these climate changes to fluctuations in atmospheric carbon dioxide. However, new research reveals the source of this carbon – and the driving forces behind it – are far more complex than previously … Read more…

Volcanoes had lower greenhouse gas emissions in Earth’s past

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The power of volcanoes to change Earth’s climate may not be as ancient as previously thought. Throughout our planet’s history, the climate has fluctuated between “icehouse” and “greenhouse” conditions, largely determined by the levels of greenhouse gases, such as carbon dioxide, in the atmosphere. Volcanic arcs, the giant chains of erupting peaks in places like … Read more…

Mid-Proterozoic expansion of passive margins and reduction in volcanic outgassing supported marine oxygenation and eukaryogenesis

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The mid-Proterozoic interval between 1800 and 800 Ma, commonly referred to as the “Boring Billion”, was marked by the emergence of eukaryotic cells from prokaryotic ancestors, a key step in the evolution of life. This period encompassed the assembly and dispersal of two consecutive supercontinents, Nuna and Rodinia, as well as the development of extensive … Read more…

Indian Ocean carbonate compensation depth since the Late Oligocene

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The carbonate compensation depth (CCD), defined as the depth in the ocean where the supply rate of pelagic carbonate is balanced by its dissolution, provides an important parameter for estimating the amount of calcium carbonate-bound carbon that is stored in deep-sea sediments. The CCD is reasonably well-constrained across the Atlantic and Pacific oceans; however, our … Read more…

Earth’s ‘boring billion years’ created the conditions for complex life

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Sydney University Media Release, 20 October 2025 Plate tectonics played central role shaping life-supporting oceans Between 1.8 and 0.8 billion years ago, Earth’s tectonic activity locked atmospheric carbon dioxide into carbonate minerals within the oceanic crust, paving the way for oxygen-rich seas and evolving life. Source: research paper A study led by researchers from the … Read more…

Regional Carbonate Compensation Depth variability in the Pacific Ocean since the Oligocene

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Deep-sea carbonates constitute the primary deep carbon reservoir, playing a critical role in regulating the long-term global carbon cycle. Reconstructing the temporal evolution of carbonate flux to the seafloor requires estimating the changes in carbonate compensation depth (CCD), a key proxy, revealing the depth where the rate of calcium carbonate supply from biogenic ooze equals … Read more…