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Geologists Demonstrate Extent Of Ancient Ice Age

June 16, 2009

Team investigates the climate of Planet Earth 440 million years ago

Geologists at the University of Leicester have shown that an ancient Ice Age, once regarded as a brief “Ëœblip’, in fact lasted for 30 million years.

They have published their findings and are due to discuss them at a public lecture at the University on Wednesday June 17.

Their research suggests that during this ancient Ice Age, global warming was curbed through the burial of organic carbon that eventually lead to the formation of oil ““ including the “Ëœhot shales’ of north Africa and Arabia which constitute the world’s most productive oil source rock.

This ice age has been named “Ëœthe Early Palaeozoic Icehouse’ by Dr Alex Page and his colleagues in a paper published as part of a collaborative Deep Time Climate project between the University of Leicester and British Geological Survey.

The Ice Age occurred in the Ordovician and Silurian Periods of geological time (part of the Early Palaeozoic Era), an interval that witnessed a major diversification of early marine animals including trilobites and primitive fish as well as the emergence of the first land plants.

The Early Palaeozoic climate had long been considered characterized by essentially greenhouse conditions with elevated atmospheric CO2 and warm temperatures extending to high latitudes, and only brief snaps of frigid climate. However, during his doctoral studies in the internationally Ârenowned Palaeobiology Research Group of the University of Leicester, Department of Geology, Alex Page and his colleagues Jan Zalasiewicz and Mark Williams demonstrated how the ice age was probably of much longer duration.

The team demonstrated that the Late Ordovician and Early Silurian Epochs were characterized by widespread ice formation, with changes in the extent of continental glaciation resulting in rapid sea level changes around the globe.

They compared evidence of sea level change from the rock record of ancient coastlines with evidence of sediments being deposited by glacial meltwaters or ice rafting at high latitudes, and with chemical indicators of temperature in the strata.

The team showed that although the Early Palaeozoic Icehouse was of similar extent and duration to the modern ice age, the workings of the carbon cycle appeared markedly different to that of the present day. Unlike the modern oceans, the oceans of the Early Palaeozoic were often oxygen-starved “Ëœdead zones’ leading to the burial of plankton-derived carbon in the sea floor sediments. The strata produced in this way include the “Ëœhot shales’ of north Africa and Arabia which constitute the world’s most productive oil source rock. In fact, the burial of organic carbon derived from fossil plankton may have served to draw down CO2 from the atmosphere to promote cooling during the Early Palaeozoic Icehouse.

Page commented: “These fossil fuel-rich deposits formed during relatively warmer episodes during the Early Palaeozoic Icehouse when the partial melting of ice sheets brought about rapid sea-level rise. This melt water may have bought a massive influx of nutrients into the surface waters, allowing animals and algae to thrive and bloom in the plankton, but also altered ocean circulation, creating oxygenÂ-poor deep waters which facilitated the preservation of fragile, carbonaceous planktonic fossils. The deglacial outwash formed a less dense, low salinity “Ëœlid’ on the oceans preventing atmospheric oxygen penetrating to the seafloor. The absence of oxygen under such conditions served to shut down decay accounting for the preservation of these fossils.”

Page added that the burial of oil shales in deglacial anoxia “may have been a negative feedback mechanism that prevented runaway warming, meaning that in the Early Palaeozoic Icehouse at least, processes eventually leading to oil formation may have been the solution to the greenhouse effect.”

Alex Page’s research will be presented at the Doctoral Inaugural Lectures being held in the Ken Edwards Lecture Theatre 3, University of Leicester. Lecture time: 5.30pm-6.30pm on Wednesday June 17.

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