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Causes of ice age intensification across the Mid-Pleistocene Transition

Proceedings of the National Academy of Sciences - PNAS, 2017-12, Vol.114 (50), p.13114-13119

2017

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Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum

Nature (London), 2017-08, Vol.548 (7669), p.573-577

2017

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Eocene global warming events driven by ventilation of oceanic dissolved organic carbon

Nature (London), 2011-03, Vol.471 (7338), p.349-352

2011

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Towards a robust and consistent middle Eocene astronomical timescale

Earth and planetary science letters, 2018-03, Vol.486, p.94-107

2018

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Persistence of carbon release events through the peak of early Eocene global warmth

Nature geoscience, 2014-10, Vol.7 (10), p.748-751

2014

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Microstructural and geochemical perspectives on planktic foraminiferal preservation: “Glassy” versus “Frosty”

Geochemistry, geophysics, geosystems : G3, 2006-12, Vol.7 (12), p.Q12P19-n/a

2006

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Calcification and growth processes in planktonic foraminifera complicate the use of B/Ca and U/Ca as carbonate chemistry proxies

Earth and planetary science letters, 2016-09, Vol.449, p.372-381

2016

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An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum

Nature geoscience, 2016-08, Vol.9 (8), p.575-580

2016

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Sensitivity of ocean circulation to warming during the Early Eocene greenhouse

Proceedings of the National Academy of Sciences - PNAS, 2024-06, Vol.121 (24), p.1

2024

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Episodes of intensified biological productivity in the subtropical Atlantic Ocean during the termination of the Middle Eocene Climatic Optimum (MECO)

Paleoceanography, 2015-08, Vol.30 (8), p.1041-1058

2015

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Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion

Biogeosciences, 2023-01, Vol.20 (1), p.121-139

2023

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Onset of North Atlantic Deep Water production coincident with inception of the Cenozoic global cooling trend

Geology (Boulder), 2012-03, Vol.40 (3), p.255-258

2012

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Onset of ‘Pacific-style’ deep-sea sedimentary carbonate cycles at the mid-Pleistocene transition

Earth and planetary science letters, 2012-03, Vol.321-322, p.81-94

2012

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High latitude regulation of low latitude thermocline ventilation and planktic foraminifer populations across glacial–interglacial cycles

Earth and planetary science letters, 2011-11, Vol.311 (1), p.69-81

2011

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Time-scale uncertainty of abrupt events in the geologic record arising from unsteady sedimentation

Geology (Boulder), 2014-10, Vol.42 (10), p.891-894

2014

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Insensitivity of alkenone carbon isotopes to atmospheric CO2 at low to moderate CO2 levels

Climate of the past, 2019-03, Vol.15 (2), p.539-554

2019

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No extreme bipolar glaciation during the main Eocene calcite compensation shift

Nature (London), 2007-08, Vol.448 (7156), p.908-911

2007

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Dispersal and biogeography of marine plankton: Long-distance dispersal of the foraminifer Truncorotalia truncatulinoides

Geology (Boulder), 2008-11, Vol.36 (11), p.899

2008

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Iterative evolution of digitate planktonic foraminifera

Paleobiology, 2007-12, Vol.33 (4), p.495-516

2007

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Sensitivity of clumped isotope temperatures in fossil benthic and planktic foraminifera to diagenetic alteration

Geochimica et cosmochimica acta, 2019-07, Vol.257 (C), p.354-372

2019

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Cenozoic North Atlantic deep circulation history recorded in contourite drifts, offshore Newfoundland, Canada

Marine geology, 2017-03, Vol.385, p.185-203

2017

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Late Maastrichtian carbon isotope stratigraphy and cyclostratigraphy of the Newfoundland Margin (Site U1403, IODP Leg 342)

Newsletters on stratigraphy, 2018-03, Vol.51 (2), p.245-260

2018

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Early Eocene Ocean Meridional Overturning Circulation: The Roles of Atmospheric Forcing and Strait Geometry

Paleoceanography and Paleoclimatology, 2022-03, Vol.37 (3), p.n/a

2022

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North Atlantic surface ocean warming and salinization in response to middle Eocene greenhouse warming

Science advances, 2023-01, Vol.9 (4), p.eabq0110

2023

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Insensitivity of alkenone carbon isotopes to atmospheric CO 2 at low to moderate CO 2 levels

Climate of the past, 2019-03, Vol.15 (2), p.539-554

2019

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Causes of ice age intensification across the Mid-Pleistocene Transition

Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum

Eocene global warming events driven by ventilation of oceanic dissolved organic carbon

Towards a robust and consistent middle Eocene astronomical timescale

Persistence of carbon release events through the peak of early Eocene global warmth

Microstructural and geochemical perspectives on planktic foraminiferal preservation: “Glassy” versus “Frosty”

Calcification and growth processes in planktonic foraminifera complicate the use of B/Ca and U/Ca as carbonate chemistry proxies

An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum

Sensitivity of ocean circulation to warming during the Early Eocene greenhouse

Episodes of intensified biological productivity in the subtropical Atlantic Ocean during the termination of the Middle Eocene Climatic Optimum (MECO)

Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion

Onset of North Atlantic Deep Water production coincident with inception of the Cenozoic global cooling trend

Onset of ‘Pacific-style’ deep-sea sedimentary carbonate cycles at the mid-Pleistocene transition

High latitude regulation of low latitude thermocline ventilation and planktic foraminifer populations across glacial–interglacial cycles

Time-scale uncertainty of abrupt events in the geologic record arising from unsteady sedimentation

Insensitivity of alkenone carbon isotopes to atmospheric CO2 at low to moderate CO2 levels

No extreme bipolar glaciation during the main Eocene calcite compensation shift

Dispersal and biogeography of marine plankton: Long-distance dispersal of the foraminifer Truncorotalia truncatulinoides

Iterative evolution of digitate planktonic foraminifera

Sensitivity of clumped isotope temperatures in fossil benthic and planktic foraminifera to diagenetic alteration

Cenozoic North Atlantic deep circulation history recorded in contourite drifts, offshore Newfoundland, Canada

Late Maastrichtian carbon isotope stratigraphy and cyclostratigraphy of the Newfoundland Margin (Site U1403, IODP Leg 342)

Early Eocene Ocean Meridional Overturning Circulation: The Roles of Atmospheric Forcing and Strait Geometry

North Atlantic surface ocean warming and salinization in response to middle Eocene greenhouse warming

Insensitivity of alkenone carbon isotopes to atmospheric CO 2 at low to moderate CO 2 levels

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