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Earth Sciences

Selected Works

Selected Works

2010

Articles 1 - 3 of 3

Full-Text Articles in Life Sciences

2,2′,5,5′-Tetra­Chloro­Benzidine, Onome Ugono, Marcel Douglas, Nigam P. Rath, Alicia M. Beatty Sep 2010

2,2′,5,5′-Tetra­Chloro­Benzidine, Onome Ugono, Marcel Douglas, Nigam P. Rath, Alicia M. Beatty

Nigam Rath

In the crystal structure of the title compound, C12H8Cl4N2, mol­ecules lie on crystallographic twofold axes at the centre of the C-C bonds linking the benzene rings, such that the asymmetric unit consists of a half-mol­ecule. The individual mol­ecules participate in inter­molecular N-H...N, N-H...Cl, C-H...Cl and Cl...Cl [3.4503 (3) Å] inter­actions.

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2,2′,5,5′-Tetra­Chloro­Benzidine, Onome Ugono, Marcel Douglas, Nigam P. Rath, Alicia M. Beatty Sep 2010

2,2′,5,5′-Tetra­Chloro­Benzidine, Onome Ugono, Marcel Douglas, Nigam P. Rath, Alicia M. Beatty

Alicia Beatty

In the crystal structure of the title compound, C12H8Cl4N2, mol­ecules lie on crystallographic twofold axes at the centre of the C-C bonds linking the benzene rings, such that the asymmetric unit consists of a half-mol­ecule. The individual mol­ecules participate in inter­molecular N-H...N, N-H...Cl, C-H...Cl and Cl...Cl [3.4503 (3) Å] inter­actions.

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Surviving Mass Extinction By Bridging The Benthic/Planktic Divide, Kate Darling, Ellen Thomas, Simone Kasemann, Heidi Seears, Christopher Smart, Christopher Wade Jan 2010

Surviving Mass Extinction By Bridging The Benthic/Planktic Divide, Kate Darling, Ellen Thomas, Simone Kasemann, Heidi Seears, Christopher Smart, Christopher Wade

Ellen Thomas

Evolution of planktic organisms from benthic ancestors is commonly thought to represent unidirectional expansion into new ecological domains, possibly only once per clade. For foraminifera, this evolutionary expansion occurred in the Early–Middle Jurassic, and all living and extinct planktic foraminifera have been placed within 1 clade, the Suborder Globigerinina. The subsequent radiation of planktic foraminifera in the Jurassic and Cretaceous resulted in highly diverse assemblages, which suffered mass extinction at the end of the Cretaceous, leaving an impoverished assemblage dominated by microperforate triserial and biserial forms. The few survivor species radiated to form diverse assemblages once again in the Cenozoic. …

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