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Attenborough Opening K. Lonsdale Building

Kathleen Lonsdale Building Re-Opened by Sir David Attenborough.

Image: Sir David Attenborough with members of Earth Sciences Department.  View the image gallery of the event on UCL Flickr
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The BBC BluePlanet

Newly discovered ocean plankton named after BBC Blue Planet.

Although measuring only thousandths of a millimetre, these plankton play a pivotal role in marine ecosystems as a crucial source of food for many ocean dwelling organisms. They are also incredibly valuable for studying the impact of climate change on ocean life now and across the previous 220 million years.
The plankton – called coccolithophores – are single cells surrounded by a calcite shell that varies drastically in shape across different species, acting as armour against predators.
“Although microscopic, the plankton are so abundant that they are visible from space as swirling blooms in the surface oceans, and form our most iconic rocks with their calcite forms making up the bulk of the white chalk cliffs and downs of southern England,” explained study co-author Professor Paul Bown.
It is the ability to produce this calcite shell that is being disrupted through ocean acidification. Ocean acidification is a symptom of climate change whereby rising atmospheric carbon dioxide is absorbed by the ocean, increasing its acidity.
By studying fossilised plankton shells or ‘coccoliths’ in samples from drilling down deep into the ocean bed, scientists can map the impact of climate change and other global events over a very long period of time and use this to inform what might happen to in the future.

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Deep-Water Research

The Ainsa Deepwater Channel Project, Spanish Pyrenees


An Integrated Outcrop Study: Project Manager: Professor Kevin T. Pickering


Introduction to the Ainsa Channel System


The Ainsa Channel System, south-central Pyrenees, occurs in the oldest part of the Campodarbe Group, and it is of Upper Eocene age. The Ainsa Channel Complex is per- haps the most famous of the submarine channel outcrops within Western Europe. The Ainsa channels consist of two principal channel complexes (Ainsa I and Ainsa II) which are separated by thin- and very thin-bedded sandy turbidites and marls. The Ainsa I Channel Complex is an example of an erosional-depositional system. The Ainsa II Chan- nel Complex contains significant erosional cut-downs, with infill of essentially non- erosive sandy facies. The channel dimensions are at a seismic scale.