Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Mills BJW"'
Autor:
van der Meer, DG, Scotese, CR, Mills, BJW, Sluijs, A, van den Berg van Saparoea, A-P, van de Weg, RMB
Global mean sea level is a key component within the fields of climate and oceanographic modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in deep time aids in our understanding of Earth’s paleoclimate and may hel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::6b9f06e95575d62e349729cbe97b8b89
https://eprints.whiterose.ac.uk/189833/7/1-s2.0-S1342937X22002192-main.pdf
https://eprints.whiterose.ac.uk/189833/7/1-s2.0-S1342937X22002192-main.pdf
The carbonate carbon isotope record has been traditionally interpreted as evidence of stability in the globally integrated ratio of organic to total carbon burial from Earth's surface environments over the past ∼3.8 billion years, but recent work h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::76a35c373da9cffaed5a93bb6e623cf5
https://eprints.whiterose.ac.uk/182903/1/Planavsky_etal_AJS_2022_combined.pdf
https://eprints.whiterose.ac.uk/182903/1/Planavsky_etal_AJS_2022_combined.pdf
Autor:
Shields, GA, Mills, BJW
Although it is widely accepted that Earth’s long-term surface temperature is regulated by the mutual dependence of silicate weathering and climate on CO2, the root causes of some climatic events remain unresolved. We show here for the first time th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::38600ef7014e1895ca45eeb7cbe24ac3
https://eprints.whiterose.ac.uk/167333/1/Shields_Mills_2020_AAM.pdf
https://eprints.whiterose.ac.uk/167333/1/Shields_Mills_2020_AAM.pdf
Autor:
Planavsky, NJ, Crowe, SA, Fakhraee, M, Beaty, B, Reinhard, CT, Mills, BJW, Holstege, C, Konhauser, KO
Life on Earth has existed for over 3.5 billion years and has caused fundamental changes in Earth’s biogeochemistry. However, the timing and impact of major events in the evolution of the biosphere are hotly contested, owing partially to the inheren
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::721b7df9e564ed83d9fb5cb71b7a1ab2
https://eprints.whiterose.ac.uk/170902/1/Planavsky_etal_2021_NREE_AAM.pdf
https://eprints.whiterose.ac.uk/170902/1/Planavsky_etal_2021_NREE_AAM.pdf
Reconciling proxy records and models of Earth's oxygenation during the Neoproterozoic and Palaeozoic
Autor:
Tostevin, R, Mills, BJW
A hypothesized rise in oxygen levels in the Neoproterozoic, dubbed the Neoproterozoic Oxygenation Event, has been repeatedly linked to the origin and rise of animal life. However, a new body of work has emerged over the past decade that questions thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::07bdaf8d3b8bd4360d549e42ac89fd87
https://eprints.whiterose.ac.uk/165529/1/Tostevin_Interface_AAM.pdf
https://eprints.whiterose.ac.uk/165529/1/Tostevin_Interface_AAM.pdf
Records suggest that the Permo–Triassic mass extinction (PTME) involved one of the most severe terrestrial ecosystem collapses of the Phanerozoic. However, it has proved difficult to constrain the extent of the primary productivity loss on land, hi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1064::5e24ff83abcfa9adebe73d6e9037bf08
https://ora.ox.ac.uk/objects/uuid:635cbb00-8ae5-4280-b9d7-d853bd987286
https://ora.ox.ac.uk/objects/uuid:635cbb00-8ae5-4280-b9d7-d853bd987286
Autor:
Capriolo, M, Marzoli, A, Aradi, LE, Callegaro, S, Dal Corso, J, Newton, RJ, Mills, BJW, Wignall, PB, Bartoli, O, Baker, DR, Youbi, N, Remusat, L, Spiess, R, Szabó, C
Large Igneous Province eruptions coincide with many major Phanerozoic mass extinctions, suggesting a cause-effect relationship where volcanic degassing triggers global climatic changes. In order to fully understand this relationship, it is necessary
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::1a7395bdc0bd33740c185183eadc3254
https://eprints.whiterose.ac.uk/157988/8/s41467-020-15325-6.pdf
https://eprints.whiterose.ac.uk/157988/8/s41467-020-15325-6.pdf
Autor:
Shields, GA, Mills, BJW
A different approach is proposed here to solve the problem of negative chemostratigraphic excursions during the Ediacárico, considering them in terms of a linked system of carbon-sulfide-oxygen, in which changes in the dynamics of oxidants would cau
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::9c03337411fec4df531323dc9d0f138e
https://eprints.whiterose.ac.uk/154942/1/1007-3095-1-PB.pdf
https://eprints.whiterose.ac.uk/154942/1/1007-3095-1-PB.pdf
Autor:
Witts, JD, Newton, RJ, Mills, BJW, Wignall, PB, Bottrell, SH, Hall, JLO, Francis, JE, Crame, JA
The Cretaceous–Paleogene (K–Pg) mass extinction event 66 million years ago led to large changes to the global carbon cycle, primarily via a decrease in primary or export productivity of the oceans. However, the effects of this event and longer-te
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9befb9081c6461a18bd706af8218dd88
https://eprints.whiterose.ac.uk/128418/9/1-s2.0-S0016703718301194-main.pdf
https://eprints.whiterose.ac.uk/128418/9/1-s2.0-S0016703718301194-main.pdf
Fossil evidence from the Rhynie chert indicates that early land plants, which evolved in a high-CO2 atmosphere during the Palaeozoic Era, hosted diverse fungal symbionts. It is hypothesized that the rise of early non-vascular land plants, and the lat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::25755f751dc9e5e031200b7289050a30
https://eprints.whiterose.ac.uk/119878/11/20160503.full.pdf
https://eprints.whiterose.ac.uk/119878/11/20160503.full.pdf