Articles | Volume 17, issue 6
https://doi.org/10.5194/cp-17-2393-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-2393-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
25 Nov 2021
Research article |
| 25 Nov 2021
| 25 Nov 2021
Maastrichtian–Rupelian paleoclimates in the southwest Pacific – a critical re-evaluation of biomarker paleothermometry and dinoflagellate cyst paleoecology at Ocean Drilling Program Site 1172
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
Joost Frieling
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
now at: Department of Earth Sciences, University of Oxford, South Parks Road OX1 3AN, Oxford, UK
Marlow Julius Cramwinckel
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
now at: School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Christine Boschman
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
Appy Sluijs
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
Francien Peterse
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
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- Eocene-Oligocene southwest Pacific Ocean paleoceanography new insights from foraminifera chemistry (DSDP site 277, Campbell Plateau) F. Hodel et al. 10.3389/feart.2022.998237
23 citations as recorded by crossref.
- Assessment of branched glycerol monoalkyl glycerol tetraether (brGMGT)-based paleothermometry in the 250,000-year sediment record of Lake Chala, equatorial East Africa A. Baxter et al. 10.1016/j.orggeochem.2024.104812
- Integrated record of the Late Lutetian Thermal Maximum at IODP site U1508, Tasman Sea: The deep-sea response I. Peñalver-Clavel et al. 10.1016/j.marmicro.2024.102390
- Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM) M. Jones et al. 10.5194/cp-19-1623-2023
- High Arctic late Paleocene and early Eocene dinoflagellate cysts A. Sluijs & H. Brinkhuis 10.5194/jm-43-441-2024
- Large and rapid salinity fluctuations affected the eastern Mediterranean at the Tortonian–Messinian transition E. Besiou et al. 10.1016/j.palaeo.2024.112568
- Revisiting the Geographical Extent of Exceptional Warmth in the Early Paleogene Southern Ocean J. Frieling et al. 10.1029/2022PA004529
- Environmental controls on the distribution of brGDGTs and brGMGTs across the Seine River basin (NW France): implications for bacterial tetraethers as a proxy for riverine runoff Z. Zhang et al. 10.5194/bg-21-2227-2024
- Eocene to Oligocene vegetation and climate in the Tasmanian Gateway region were controlled by changes in ocean currents and <i>p</i>CO<sub>2</sub> M. Amoo et al. 10.5194/cp-18-525-2022
- Biostratigraphy, paleoenvironment and paleoclimate in northeastern Patagonia during the early Paleocene based on the micropaleontological record M. Estebenet et al. 10.1016/j.eve.2024.100052
- Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world C. Fokkema et al. 10.5194/cp-20-1303-2024
- Late Paleocene CO<sub>2</sub> drawdown, climatic cooling and terrestrial denudation in the southwest Pacific C. Hollis et al. 10.5194/cp-18-1295-2022
- Heterotrophic origin and diverse sources of branched glycerol monoalkyl glycerol tetraethers (brGMGTs) in peats and lignites F. Elling et al. 10.1016/j.orggeochem.2023.104558
- Resilient Antarctic monsoonal climate prevented ice growth during the Eocene M. Baatsen et al. 10.5194/cp-20-77-2024
- The temperature-precipitation duel and tropical greening during the Early Eocene Greenhouse episode A. Samanta et al. 10.1016/j.gloplacha.2024.104603
- Late Eocene to late Oligocene terrestrial climate and vegetation change in the western Tasmanian region M. Amoo et al. 10.1016/j.palaeo.2023.111632
- Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene D. Jenny et al. 10.5194/cp-20-1627-2024
- Distinct sources of bacterial branched GMGTs in the Godavari River basin (India) and Bay of Bengal sediments F. Kirkels et al. 10.1016/j.orggeochem.2022.104405
- Lipid-biomarker-based sea surface temperature record offshore Tasmania over the last 23 million years S. Hou et al. 10.5194/cp-19-787-2023
- Ice sheet–free West Antarctica during peak early Oligocene glaciation J. Klages et al. 10.1126/science.adj3931
- Impact of organic carbon reworking upon GDGT temperature proxies during the Paleocene-Eocene Thermal Maximum G. Inglis et al. 10.1016/j.orggeochem.2023.104644
- Climatic controls on water-mass chemistry in a Paleocene lacustrine setting, Subei Basin, eastern China Y. Liu et al. 10.1130/B37455.1
- Late Miocene cooling and uplift recorded by bacterial H-GDGTs in the Xining Basin, northeastern Tibetan Plateau Y. Huang et al. 10.1016/j.palaeo.2024.112354
- The Paleocene - Eocene mangroves of southeastern Australia: spatial and temporal occurrences across four geological basins G. Holdgate et al. 10.1016/j.palaeo.2024.112317
3 citations as recorded by crossref.
- The PhanSST global database of Phanerozoic sea surface temperature proxy data E. Judd et al. 10.1038/s41597-022-01826-0
- Strength and variability of the Oligocene Southern Ocean surface temperature gradient F. Hoem et al. 10.1038/s43247-022-00666-5
- Eocene-Oligocene southwest Pacific Ocean paleoceanography new insights from foraminifera chemistry (DSDP site 277, Campbell Plateau) F. Hodel et al. 10.3389/feart.2022.998237
Latest update: 13 Dec 2024
Short summary
Here, we use the latest insights for GDGT and dinocyst-based paleotemperature and paleoenvironmental reconstructions in late Cretaceous–early Oligocene sediments from ODP Site 1172 (East Tasman Plateau, Australia). We reconstruct strong river runoff during the Paleocene–early Eocene, a progressive decline thereafter with increased wet/dry seasonality in the northward-drifting hinterland. Our critical review leaves the anomalous warmth of the Eocene SW Pacific Ocean unexplained.
Here, we use the latest insights for GDGT and dinocyst-based paleotemperature and...
