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Disentangling rock record bias and common-cause from redundancy in the British fossil record

Palaeodiversity estimations are confounded by fossil availability and sampling. Here, Dunhill et al.use the fossil record of Great Britain to test aspects of the marine and terrestrial fossil records that are commonly used to identify and correct for bias in palaeodiversity estimations.

Alexander M. Dunhill
Bjarte Hannisdal
Michael J. Benton
ResearchOpen Access04 Sept 2014
Nature Communications

Volume: 5, P: 1-9
Eurasian Ice Sheet collapse was a major source of Meltwater Pulse 1A 14,600 years ago

Marine-based sections of the Eurasian Ice Sheet collapsed rapidly during a warming event 14,600 years ago and contributed to the Meltwater Pulse 1A event, according to a recalibrated age model for sediments from the Norwegian Sea.

Jo Brendryen
Haflidi Haflidason
Bjarte Hannisdal
Research20 Apr 2020
Nature Geoscience

Volume: 13, P: 363-368
Forcing of late Pleistocene ice volume by spatially variable summer energy

Kristian Agasøster Haaga
Jo Brendryen
Bjarte Hannisdal
ResearchOpen Access01 Aug 2018
Scientific Reports

Volume: 8, P: 1-10
Nitrifier abundance and diversity peak at deep redox transition zones

Rui Zhao
Bjarte Hannisdal
Steffen L. Jørgensen
ResearchOpen Access14 Jun 2019
Scientific Reports

Volume: 9, P: 1-12
Distinct microbial communities associated with buried soils in the Siberian tundra

Antje Gittel
Jiří Bárta
Tim Urich
Research12 Dec 2013
The ISME Journal

Volume: 8, P: 841-853

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Disentangling rock record bias and common-cause from redundancy in the British fossil record

Eurasian Ice Sheet collapse was a major source of Meltwater Pulse 1A 14,600 years ago

Forcing of late Pleistocene ice volume by spatially variable summer energy

Nitrifier abundance and diversity peak at deep redox transition zones

Distinct microbial communities associated with buried soils in the Siberian tundra

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