Articles | Volume 13, issue 9
https://doi.org/10.5194/bg-13-2859-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-2859-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Equatorward phytoplankton migration during a cold spell within the Late Cretaceous super-greenhouse
Niels A. G. M. van Helmond
CORRESPONDING AUTHOR
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
Appy Sluijs
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
Nina M. Papadomanolaki
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
A. Guy Plint
Department of Earth Sciences, The University of Western Ontario,
London, Ontario N6A 5B7, Canada
Darren R. Gröcke
Department of Earth Sciences, Durham University, South Road, Durham
DH1 3LE, UK
Martin A. Pearce
Evolution Applied Ltd, 50 Mitchell Way, Upper Rissington, Cheltenham,
Gloucestershire GL54 2PL, UK
James S. Eldrett
Shell International Exploration and Production Inc., Kesslerpark 1,
2288 GS Rijswijk, the Netherlands
João Trabucho-Alexandre
Department of Earth Sciences, Durham University, South Road, Durham
DH1 3LE, UK
Comparative Sedimentology Group, Department of Earth Sciences, Faculty
of Geosciences, Utrecht University, Heidelberglaan 2, 3584 CS Utrecht, the
Netherlands
Ireneusz Walaszczyk
Institute of Geology, Faculty of Geology, University of Warsaw, Zwirki
I Wigury 93, 02-089 Warsaw, Poland
Bas van de Schootbrugge
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
Henk Brinkhuis
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
NIOZ, Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790
AB Den Burg, Texel, the Netherlands
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- The Cretaceous succession of northeast Baffin Bay: Stratigraphy, sedimentology and petroleum potential H. Nøhr-Hansen et al. 10.1016/j.marpetgeo.2021.105108
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- Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid‐Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous) J. Scaife et al. 10.1002/2017GC007153
- Onset and demise of Cretaceous oceanic anoxic events: The coupling of surface and bottom oceanic processes in two pelagic basins of the western Tethys G. Gambacorta et al. 10.1002/2015PA002922
37 citations as recorded by crossref.
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- Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2 U. Heimhofer et al. 10.1038/s41467-018-06319-6
- Exploring the paleoceanographic changes registered by planktonic foraminifera across the Cenomanian-Turonian boundary interval and Oceanic Anoxic Event 2 at southern high latitudes in the Mentelle Basin (SE Indian Ocean) M. Petrizzo et al. 10.1016/j.gloplacha.2021.103595
- Models of organic enrichment in epicontinental basins: Applications of a large organic geochemical dataset from the Cretaceous Western Interior Seaway L. Robinson & J. Whiteside 10.1016/j.cretres.2022.105160
- DINOSTRAT: a global database of the stratigraphic and paleolatitudinal distribution of Mesozoic–Cenozoic organic-walled dinoflagellate cysts P. Bijl 10.5194/essd-14-579-2022
- High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin A. Plint & M. Kreitner 10.35767/gscpgbull.67.2.71
- Biostratigraphy and Inoceramus survival across the Cenomanian–Turonian (Cretaceous) boundary in the Ram River section, Alberta, Canada I. Walaszczyk et al. 10.1515/agp-2016-0039
- Palynology and calcareous nannofossil biostratigraphy of the Turonian – Coniacian boundary: The proposed boundary stratotype at Salzgitter-Salder, Germany and its correlation in NW Europe I. Jarvis et al. 10.1016/j.cretres.2021.104782
- The Cretaceous succession of northeast Baffin Bay: Stratigraphy, sedimentology and petroleum potential H. Nøhr-Hansen et al. 10.1016/j.marpetgeo.2021.105108
- Nitrogen and carbon cycle perturbations through the Cenomanian-Turonian oceanic anoxic event 2 (~94 Ma) in the Vocontian Basin (SE France) J. Danzelle et al. 10.1016/j.palaeo.2019.109443
- Two areoligeracean dinoflagellate cysts from the Carstone Formation (Lower Cretaceous) at Middlegate Quarry, North Lincolnshire, UK P. Dodsworth & R. Black 10.1144/pygs2024-004
- A dinoflagellate cyst zonation of the Cenomanian and Turonian (Upper Cretaceous) in the Western Interior, United States P. Dodsworth & J. Eldrett 10.1080/01916122.2018.1477851
- Redox conditions and ecological resilience during Oceanic Anoxic Event 2 in the Western Interior Seaway L. Robinson et al. 10.1016/j.palaeo.2023.111496
- Zinc- and cadmium-isotope evidence for redox-driven perturbations to global micronutrient cycles during Oceanic Anoxic Event 2 (Late Cretaceous) T. Sweere et al. 10.1016/j.epsl.2020.116427
- A Re‐evaluation of the Plenus Cold Event, and the Links Between CO2, Temperature, and Seawater Chemistry During OAE 2 L. O'Connor et al. 10.1029/2019PA003631
- Enhanced Arctic-Tethys connectivity ended the Toarcian Oceanic Anoxic Event in NW Europe B. van de Schootbrugge et al. 10.1017/S0016756819001262
- Evidence for changes in sea-surface circulation patterns and ~20° equatorward expansion of the Boreal bioprovince during a cold snap of Oceanic Anoxic Event 2 (Late Cretaceous) F. Falzoni & M. Petrizzo 10.1016/j.gloplacha.2021.103678
- Benthic foraminiferal response to the Oceanic Anoxic Event 2 (Late Cretaceous) and evidence of bottom water re‐oxygenation during the Plenus Cold Event at Clot Chevalier (Vocontian Basin, SE France) G. Amaglio et al. 10.1016/j.palaeo.2023.111598
- A 87Sr/86Sr, δ18O and δ13C record of Turonian-Santonian belemnites from lower Volga region of the East European Platform: Stratigraphic significance and palaeoenvironmental reconstructions Y. Zakharov et al. 10.1016/j.geobios.2022.07.006
- Timing of the Greenhorn transgression and OAE2 in Central Utah using CA-TIMS U-Pb zircon dating R. Renaut et al. 10.1016/j.cretres.2022.105464
- Isotopic evidence for changes in the zinc cycle during Oceanic Anoxic Event 2 (Late Cretaceous) T. Sweere et al. 10.1130/G40226.1
- Low-latitude ?upper Barremian–lower Aptian palynoflora and paleovegetation of the Biyadh Formation (Arabian Plate, eastern margin of northern Gondwana): evidence for a possible cold snap H. Boukhamsin et al. 10.1016/j.cretres.2021.104995
- High resolution osmium data record three distinct pulses of magmatic activity during cretaceous Oceanic Anoxic Event 2 (OAE-2) D. Sullivan et al. 10.1016/j.gca.2020.04.002
- A new record of the Cenomanian–Turonian transgression preserved in the Ikorfat Fault zone, Nuussuaq Basin, West Greenland G. Pedersen et al. 10.1016/j.cretres.2023.105481
- Statistical approaches for improved definition of carbon isotope excursions J. Eldrett et al. 10.1016/j.earscirev.2024.104851
- Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian, Late Cretaceous) H. Jenkyns et al. 10.1111/sed.12305
- Cretaceous large igneous provinces: from volcanic formation to environmental catastrophes and biological crises L. Percival et al. 10.1144/SP544-2023-88
- High‐frequency sequences within a retrogradational deltaic succession: Upper Cenomanian Dunvegan Formation, Western Canada Foreland Basin M. Hay & A. Plint 10.1002/dep2.114
- Late Cenomanian Plenus event in the Western Interior Seaway B. Sageman et al. 10.1016/j.cretres.2023.105798
- Comparing Seawater Temperature Proxy Records for the Past 90 Myrs From the Shallow Shelf Record Bass River, New Jersey M. de Bar et al. 10.1029/2018PA003453
- The expression of late Cenomanian–Coniacian episodes of accelerated global change in the sedimentary record of the Mexican Interior Basin A. Colín-Rodríguez et al. 10.1016/j.cretres.2022.105380
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- Spatial heterogeneity in benthic foraminiferal assemblages tracks regional impacts of paleoenvironmental change across Cretaceous OAE2 R. Bryant & C. Belanger 10.1017/pab.2022.47
- Anatomy of a late Cenomanian transgressive shelf system: The influence of high-frequency eustasy and crustal flexure on stratigraphy and paleogeography, basal Kaskapau Formation, Western Canada Foreland Basin A. Plint 10.35767/gscpgbull.67.1.1
- Patterns of planktonic foraminiferal extinctions and eclipses during Oceanic Anoxic Event 2 at Eastbourne (SE England) and other mid-low latitude locations F. Falzoni & M. Petrizzo 10.1016/j.cretres.2020.104593
- Lead-up and manifestation of the Oceanic Anoxic Event 2 at the DSDP Site 398 (Vigo Seamount, NW Iberian offshore): Palynological and geochemical insights I. Rodríguez-Barreiro et al. 10.1016/j.palaeo.2024.112223
- Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid‐Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous) J. Scaife et al. 10.1002/2017GC007153
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Latest update: 23 Nov 2024
Short summary
Over the past decades large changes have been observed in the biogeographical dispersion of marine life resulting from climate change. To better understand present and future trends it is important to document and fully understand the biogeographical response of marine life during episodes of environmental change in the geological past.
Here we investigate the response of phytoplankton, the base of the marine food web, to a rapid cold spell, interrupting greenhouse conditions during the Cretaceous.
Over the past decades large changes have been observed in the biogeographical dispersion of...
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