Zobrazeno 1 - 10
of 67
pro vyhledávání: '"Jorijntje Henderiks"'
Publikováno v:
Journal of Marine Science and Engineering, Vol 10, Iss 6, p 798 (2022)
Haptophytes are photosynthetic protists found in both freshwater and marine environments with an origin possibly dating back to the Neoproterozoic era. The most recent molecular phylogeny reveals several haptophyte “mystery clades” that await mor
Externí odkaz:
https://doaj.org/article/942d981a7f9242bd880174929e314457
Late Miocene to Pliocene sediments from the NW Australian shelf, drilled by the International Ocean Discovery Program (IODP) Expedition 356, provide unique records of paleoclimatic variations under warmer-than-present conditions. During the period fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76a44f6cebd6d90250a9d543efa0430e
https://cp.copernicus.org/articles/19/765/2023/
https://cp.copernicus.org/articles/19/765/2023/
Autor:
Jorijntje Henderiks
Publikováno v:
Science (New York, N.Y.). 376(6595)
Marine phytoplankton show notable resilience during extreme ocean states
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7cc081d4c31b87e54321159a583feda1
https://pubmed.ncbi.nlm.nih.gov/35587965
https://pubmed.ncbi.nlm.nih.gov/35587965
Publikováno v:
Geochimica et Cosmochimica Acta. 281:118-134
Haptophyte algal biomarkers called alkenones are widely used to reconstruct atmospheric CO2 in Earth’s Cenozoic history. This method is based on the notion that the algal carbon isotope fractionation during photosynthesis, as represented by ep37:2,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f26fa1e843a10100ee376f1885fd9e05
https://doi.org/10.1016/j.gca.2020.05.002
https://doi.org/10.1016/j.gca.2020.05.002
The late Miocene to early Pliocene was a time of global cooling, albeit in a warmer-than present climate state. Increased marine primary productivity characterizes this interval, often referred to as the late Miocene-early Pliocene biogenic bloom (~9
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b053f24cba1d81f15d202f486250d6fe
https://doi.org/10.5194/egusphere-egu21-10071
https://doi.org/10.5194/egusphere-egu21-10071
Autor:
Sarah J. Feakins, Helen K. Coxall, A. M. de Boer, Matthew Huber, Gregor Knorr, Natalie J. Burls, Jorijntje Henderiks, Heather Stoll, Matthew J. Kohn, Wolfram M. Kürschner, Daniel J. Lunt, Margret Steinthorsdottir, Matthew J. Pound, Natasha Barbolini, Caroline H Lear, Paul Nicholas Pearson, S. Kiel, Diederik Liebrand, Catherine Bradshaw, Thomas Mörs, Ann Holbourn, Caroline A.E. Strömberg, Edward Gasson
Publikováno v:
e2020PA004037
Paleoceanography and Paleoclimatology
Steinthorsdottir, M, Coxall, H K, de Boer, A M, Huber, M, Barbolini, N, Bradshaw, C D, Burls, N J, Feakins, S J, Gasson, E, Henderiks, J, Holbourn, A E, Kiel, S, Kohn, M J, Knorr, G, Kürschner, W M, Lear, C H, Liebrand, D, Lunt, D J, Mörs, T, Pearson, P N, Pound, M J, Stoll, H & Strömberg, C A E 2021, ' The Miocene : The Future of the Past ', Paleoceanography and Paleoclimatology, vol. 36, no. 4, e2020PA004037 . https://doi.org/10.1029/2020PA004037
Paleoceanography and Paleoclimatology, 36 (4)
Paleoceanography and Paleoclimatology
Steinthorsdottir, M, Coxall, H K, de Boer, A M, Huber, M, Barbolini, N, Bradshaw, C D, Burls, N J, Feakins, S J, Gasson, E, Henderiks, J, Holbourn, A E, Kiel, S, Kohn, M J, Knorr, G, Kürschner, W M, Lear, C H, Liebrand, D, Lunt, D J, Mörs, T, Pearson, P N, Pound, M J, Stoll, H & Strömberg, C A E 2021, ' The Miocene : The Future of the Past ', Paleoceanography and Paleoclimatology, vol. 36, no. 4, e2020PA004037 . https://doi.org/10.1029/2020PA004037
Paleoceanography and Paleoclimatology, 36 (4)
The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continental configurations and mountain topography transitioned toward modern conditions, and many flora and fauna evolved into the same taxa that exist toda
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f5e859026e89ce61a82979e3d9f936ca
http://hdl.handle.net/10852/85961
http://hdl.handle.net/10852/85961
Autor:
Gerald Auer, R. A. Smith, Kara Bogus, Stephen J. Gallagher, Isla S. Castañeda, Beth A Christensen, Jeroen Groeneveld, Willem Renema, Jorijntje Henderiks, David De Vleeschouwer, Craig S. Fulthorpe
Publikováno v:
Paleoceanography and Paleoclimatology. 35
Ocean gateways facilitate circulation between ocean basins, thereby impacting global climate. The Indonesian Gateway transports water from the Pacific to the Indian Ocean via the Indonesian Throughflow (ITF) and drives the strength and intensity of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba1a828698d2c98791b72703d720174b
https://doi.org/10.1029/2020pa003872
https://doi.org/10.1029/2020pa003872
Autor:
Jeroen Groeneveld, David De Vleeschouwer, Beth A Christensen, B.‐Th. Karatsolis, Jorijntje Henderiks
Publikováno v:
Paleoceanography and Paleoclimatology. 35
Pre-Quaternary paleoclimate studies in Australia mainly focus on terrestrial records from the southeastern part of the continent. IODP Expedition 356 drilled on the northwestern Australian shelf, yielding Miocene-Pleistocene paleoclimate records in a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::978e98233935599394058869ecc804fb
https://doi.org/10.1029/2019pa003780
https://doi.org/10.1029/2019pa003780
Autor:
Anna Joy Drury, Beth A Christensen, Jeroen Groeneveld, Jorijntje Henderiks, Gregor P. Eberli, Gerald Auer, David DeVleeschouwer, Christian Beztler, Dirk Kroon
The recent documentation of the southern hemisphere “supergyre”, the coupled subtropical southern hemisphere gyres spanning the 3 ocean basins, leads to questions about its impact on Indian Ocean circulation. The Indonesian Throughflow (ITF) acts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::accd5e04fcffb9b2b7c0bcecdce97e74
https://doi.org/10.5194/egusphere-egu2020-11701
https://doi.org/10.5194/egusphere-egu2020-11701