The micropaleontology group studies variation within the distribution and community structure amongst microfossils from completely different environmental conditions and from completely different durations. As a result of their abundance and sensitivity to totally different parameters, diatoms play a key role in Paleoceanography, particularly for proof of climatic cooling and altering sedimentation charges in the Arctic and Antarctic oceans and to estimate sea floor temperature.
The collections , with more than 20,000 samples, cover 4 microfossil teamscalcareous nannofossils, foraminifers, radiolarians, and diatomschosen from sediment cores obtained from the Deep Sea Drilling Project (DSDP), the Ocean Drilling Program (ODP), and the Integrated Ocean Drilling Program (IODP).
Microfossils are especially noteworthy for their significance in biostratigraphy Since microfossils are often extraordinarily abundant, widespread, and fast to seem and disappear from the stratigraphic record, they constitute ultimate index fossils from a biostratigraphic perspective.
Sediment or rock samples are collected from both cores or outcrops, and the microfossils they contain are extracted by a variety of bodily and chemical laboratory methods, together with sieving, density separation by centrifuge or in heavy liquids, and chemical digestion of the unwanted fraction.
Throughout the Late Cretaceous the worldwide climate change has been associated with episodes of outgassing from major volcanic occasions, orbital cyclicity and tectonism earlier than ending with the cataclysm caused by a big bolide impression at Chicxulub, on the Yucatán Peninsula, Mexico.