Earth’s climate system is connected across hemispheres. When the Atlantic Meridional Overturning Circulation weakens and Europe cools, warming in New Zealand and southern mid-latitudes accelerates.
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Fossil evidence of how the earliest life on Earth came to be is hard to come by. But scientists have come up with a few theories based on the microbes, viruses and prions existing today.
Microfossils offer up an array of information to scientists, like the time periods in which they lived and how environments have changed.
New research shows how rock features that look like fossilised microbes can form without life.
Kontributor teratas
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Senior Lecturer in Geology, University of Aberdeen
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Senior Lecturer, North-West University
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PhD candidate in Sedimentology, University of the Western Cape
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Professor Emeritus of Microbiology, University of Connecticut
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Chief Investigator in Antarctic environmental science, Monash University
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Senior Lecturer in Physical Geography, Te Herenga Waka — Victoria University of Wellington
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Associate Professor in Marine Geology, The University of Queensland
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Palaeoclimatologist, Australian Antarctic Division
