16 March 2012
The growth rate of the Earth’s continental crust was high during the first 1.5 billion years of the planet’s history then decreased markedly for the next 3 billion years to the present day, according to new research from the University of Bristol, published today [16 March] in Science. This sharp decrease indicates a dramatic change in the way the continental crust was generated and preserved.
The Earth is around 4.5 billion years old. At present 75 per cent of the continental crust – the crust we live on – is less than 1 billion years old, and only around 7 per cent of it is made up of rocks of Archaean age (that is older than 2.5 billion years).
What is striking, and perhaps unexpected, is that there is increasing evidence that large volumes of continental crust were generated before 2.5 billion years ago. Thus the distribution of rocks of different ages in the continental crust was very different back in time, because of the repeated interactions between the crust, and the convecting mantle from which the crust was generated. As a consequence, the timing, rates and the geodynamical conditions of continental crust generation, destruction and reworking remain a topic of considerable debate.
To understand when the continental crust was generated it is important to establish the proportions of new continental crust and of crust reworked through erosion and sedimentation, and through partial melting.
To do this, Dr Bruno Dhuime of Bristol’s School of Earth Sciences with colleagues from the Universities of St Andrews and Portsmouth, studied the oxygen isotopic composition of zircons in the Earth’s crust using data generated at the Bristol Isotope Group and compiled from the literature. The ages of zircon, a mineral commonly found in granitic rocks and in clastic sediments of various ages, can be determined to high precision, and these ages remain the basic chronological framework of the history of the Earth.
Read the full story on the University News page.