Malka L. Machlus
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Previous Organizations / Institutes
The organizations / institutes from the scholar's other articles in the past ten years
Research Subjects
Malka L. Machlus has a total of 130 co-authors. Here are the top co-authors by number of shared publications:
- Donna J. Shillington
School of Earth and Sustainability Northern Arizona University Flagstaff AZ USA
10 shared publications - Lisa C. McNeill
Ocean and Earth Science, National Oceanography Centre Southampton University of Southampton Southampton UK
10 shared publications - Robert L. Gawthorpe
Department of Earth Science University of Bergen Bergen Norway
10 shared publications - Sofia Pechlivanidou
Department of Earth Science, University of Bergen, Bergen, Norway
10 shared publications - Jack Gillespie
Institute of Earth Sciences, Faculty of Geosciences and Environment, University of Lausanne, Lausanne CH-1015, Switzerland
9 shared publications - Richard E. Ll. Collier
School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK
9 shared publications
Latest Publications
- Open Access
- 29 April 2025
- Published by International Ocean Discovery Program (IODP)
- Vol. 381
Data report: age-depth model of the Corinth synrift sequence, Site M0079, IODP Expedition 381
Data report: age-depth model of the Corinth synrift sequence, Site M0079, IODP Expedition 381
- 29 April 2025
- Published by International Ocean Discovery Program (IODP)
- Vol. 381
Open AccessData report: age-depth model of the Corinth synrift sequence, Site M0079, IODP Expedition 381
Data report: age-depth model of the Corinth synrift sequence, Site M0079, IODP Expedition 381
- 7 March 2025
- Published by Geological Society of America in Geological Society of America Bulletin
- Vol. 137 (7-8) , 3463-3480
Magnetostratigraphy and U-Pb geochronology of the middle Eocene Bridger Formation (Wyoming, USA): Implications for the age and correlation of the Bridgerian/Uintan NALMA boundary and calibration of the Geomagnetic Polarity Time Scale
The rich fossil record of the central Rocky Mountains has been fundamental to constructing the terrestrial biostratigraphy and biochronology that forms the basis of the North American Land Mammal “Ages” (NALMAs). New integrated magnetostratigraphy and high-precision U-Pb geochronology (chemical abrasion–isotope dilution–thermal ionization mass spectrometry [CA-ID-TIMS] method) from the middle Eocene Bridger Formation of the Bridger Basin in southwestern Wyoming, USA, provide a robust chronostratigraphic framework for the Bridgerian to earliest Uintan NALMAs. Paleomagnetic analysis of samples from 90 sites in an ~560 m composite section spanning from Bridger B through Bridger E members indicates two paleomagnetic reversals, and the section is correlated to Chrons C22n, C21r, and C21n by comparison to the Geomagnetic Polarity Time Scale (GPTS). This correlation places the Bridgerian/Uintan boundary within Chron C21n during the Early Eocene Climatic Optimum and subsequent initial cooling. Based on this bio- and magnetostratigraphic correlation, we also correlate other key Bridgerian/Uintan boundary bearing sections from the Washakie Basin and East Fork Basin to the GPTS and determine that the boundary occurs everywhere in Chron C21n in western North America. Furthermore, the Bridgerian NALMA is now estimated to have lasted for ~5 million years. Integrating this magnetostratigraphy with existing and new U-Pb zircon geochronology from the interbedded Church Butte tuff, Henrys Fork tuff, and Sage Creek Mountain tuff in the Bridger Formation permits assessment of existing age calibration models for the early-middle Eocene interval of the GPTS. Evaluation of the calibration models identifies two previously published models that best reconcile the geochronological data from the Greater Green River Basin, improving calibration accuracy of the Geomagnetic Polarity Time Scale in the early to middle Eocene.
- 7 March 2025
- Published by Geological Society of America in Geological Society of America Bulletin
- Vol. 137 (7-8) , 3463-3480
Magnetostratigraphy and U-Pb geochronology of the middle Eocene Bridger Formation (Wyoming, USA): Implications for the age and correlation of the Bridgerian/Uintan NALMA boundary and calibration of the Geomagnetic Polarity Time Scale
The rich fossil record of the central Rocky Mountains has been fundamental to constructing the terrestrial biostratigraphy and biochronology that forms the basis of the North American Land Mammal “Ages” (NALMAs). New integrated magnetostratigraphy and high-precision U-Pb geochronology (chemical abrasion–isotope dilution–thermal ionization mass spectrometry [CA-ID-TIMS] method) from the middle Eocene Bridger Formation of the Bridger Basin in southwestern Wyoming, USA, provide a robust chronostratigraphic framework for the Bridgerian to earliest Uintan NALMAs. Paleomagnetic analysis of samples from 90 sites in an ~560 m composite section spanning from Bridger B through Bridger E members indicates two paleomagnetic reversals, and the section is correlated to Chrons C22n, C21r, and C21n by comparison to the Geomagnetic Polarity Time Scale (GPTS). This correlation places the Bridgerian/Uintan boundary within Chron C21n during the Early Eocene Climatic Optimum and subsequent initial cooling. Based on this bio- and magnetostratigraphic correlation, we also correlate other key Bridgerian/Uintan boundary bearing sections from the Washakie Basin and East Fork Basin to the GPTS and determine that the boundary occurs everywhere in Chron C21n in western North America. Furthermore, the Bridgerian NALMA is now estimated to have lasted for ~5 million years. Integrating this magnetostratigraphy with existing and new U-Pb zircon geochronology from the interbedded Church Butte tuff, Henrys Fork tuff, and Sage Creek Mountain tuff in the Bridger Formation permits assessment of existing age calibration models for the early-middle Eocene interval of the GPTS. Evaluation of the calibration models identifies two previously published models that best reconcile the geochronological data from the Greater Green River Basin, improving calibration accuracy of the Geomagnetic Polarity Time Scale in the early to middle Eocene.
- Open Access
- 19 April 2019
- Published by Springer Nature in Scientific Reports
- Vol. 9 (1) , 6519
Author Correction: High-resolution record reveals climate-driven environmental and sedimentary changes in an active rift
A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper.
- 19 April 2019
- Published by Springer Nature in Scientific Reports
- Vol. 9 (1) , 6519
Open AccessAuthor Correction: High-resolution record reveals climate-driven environmental and sedimentary changes in an active rift
A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper.
- Open Access
- 28 February 2019
- Published by International Ocean Discovery Program (IODP)
Expedition 381 methods
- 28 February 2019
- Published by International Ocean Discovery Program (IODP)
Open AccessExpedition 381 methods
- Open Access
- 28 February 2019
- Published by International Ocean Discovery Program (IODP)
Expedition 381 summary
- 28 February 2019
- Published by International Ocean Discovery Program (IODP)
Open AccessExpedition 381 summary
- Open Access
- 28 February 2019
- Published by International Ocean Discovery Program (IODP)
Expedition 381 facies associations
Expedition 381 facies associations
- 28 February 2019
- Published by International Ocean Discovery Program (IODP)
Open AccessExpedition 381 facies associations
Expedition 381 facies associations