scholarly journals Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years

2014 ◽  
Vol 111 (12) ◽  
pp. E1062-E1063 ◽  
Author(s):  
R. E. Zeebe ◽  
G. R. Dickens ◽  
A. Ridgwell ◽  
A. Sluijs ◽  
E. Thomas
2016 ◽  
Vol 128 (9-10) ◽  
pp. 1352-1366 ◽  
Author(s):  
Allison A. Baczynski ◽  
Francesca A. McInerney ◽  
Scott L. Wing ◽  
Mary J. Kraus ◽  
Paul E. Morse ◽  
...  

2019 ◽  
Vol 10 (1) ◽  
Author(s):  
Felix J. Elling ◽  
Julia Gottschalk ◽  
Katiana D. Doeana ◽  
Stephanie Kusch ◽  
Sarah J. Hurley ◽  
...  

Abstract A negative carbon isotope excursion recorded in terrestrial and marine archives reflects massive carbon emissions into the exogenic carbon reservoir during the Paleocene-Eocene Thermal Maximum. Yet, discrepancies in carbon isotope excursion estimates from different sample types lead to substantial uncertainties in the source, scale, and timing of carbon emissions. Here we show that membrane lipids of marine planktonic archaea reliably record both the carbon isotope excursion and surface ocean warming during the Paleocene-Eocene Thermal Maximum. Novel records of the isotopic composition of crenarchaeol constrain the global carbon isotope excursion magnitude to −4.0 ± 0.4‰, consistent with emission of >3000 Pg C from methane hydrate dissociation or >4400 Pg C for scenarios involving emissions from geothermal heating or oxidation of sedimentary organic matter. A pre-onset excursion in the isotopic composition of crenarchaeol and ocean temperature highlights the susceptibility of the late Paleocene carbon cycle to perturbations and suggests that climate instability preceded the Paleocene-Eocene Thermal Maximum.


2014 ◽  
Vol 10 (4) ◽  
pp. 3303-3325 ◽  
Author(s):  
P. N. Pearson ◽  
E. Thomas

Abstract. The onset of the Paleocene/Eocene thermal maximum (PETM) and associated carbon isotope excursion (CIE; about 56 million years ago) was geologically abrupt but it is debated whether it took thousands of years or was effectively instantaneous. A significant new record of the onset of the CIE was published by Wright and Schaller (2013) who claimed that it could be resolved across 13 annual layers in a drill core through the Marlboro Clay at Millville, New Jersey (Ocean Drilling Program Leg 174X). Supporting evidence of similar layering was also reported from another New Jersey drill site, Wilson Lake B, and a photograph of the Marlboro Clay in outcrop. Such a short duration would imply an instantaneous perturbation of the atmosphere and surface ocean, and the impact of a comet or asteroid as the likely cause. However it was suggested by Pearson and Nicholas (2014) from the published photographs that the layers in the Marlboro Clay could be artifacts of drilling disturbance (so-called "biscuiting", wherein the formation is fractured into layers or "biscuits" and drilling mud is injected in between). Here we report new observations on the cores which support that interpretation, including concentric grooves on the surfaces of the biscuits caused by spinning in the bit, micro-fracturing at their edges, and injected drilling mud. We re-interpret the outcrop evidence as showing joints rather than sedimentary layers. We argue that foraminifer concentrations in the sediments are far too high for the layers to be annually deposited in turbid waters at depths of 40–70 m, indicating that the onset of the CIE in the Marlboro Clay likely took on the order of millennia, not years. Re-coring of Millville to minimize drilling disturbance and allow a higher resolution study of the carbon isotope excursion is highly desirable.


2013 ◽  
Vol 14 (10) ◽  
pp. 4133-4152 ◽  
Author(s):  
Allison A. Baczynski ◽  
Francesca A. McInerney ◽  
Scott L. Wing ◽  
Mary J. Kraus ◽  
Jonathan I. Bloch ◽  
...  

2003 ◽  
Vol 211 (1-2) ◽  
pp. 13-26 ◽  
Author(s):  
D.V. Kent ◽  
B.S. Cramer ◽  
L. Lanci ◽  
D. Wang ◽  
J.D. Wright ◽  
...  

2015 ◽  
Vol 11 (1) ◽  
pp. 95-104 ◽  
Author(s):  
P. N. Pearson ◽  
E. Thomas

Abstract. The onset of the Paleocene–Eocene thermal maximum (PETM) and associated carbon isotope excursion (CIE; approx. 56 Mya) was geologically abrupt, but it is debated whether it took thousands of years or was effectively instantaneous. Wright and Schaller (2013) published a significant new record of the onset of the CIE, and claimed that it could be resolved across 13 annual layers in a drill core through the Marlboro clay at Millville, New Jersey (Ocean Drilling Program (ODP) Leg 174X). Supporting evidence for similar layering was reported from another New Jersey drill site, Wilson Lake B, and a photograph of the Marlboro clay in outcrop (Wright and Schaller, 2014). Such a short duration would imply an instantaneous perturbation of the atmosphere and surface ocean and the impact of a comet or asteroid as the likely cause. However, Pearson and Nicholas (2014) suggested, based on the published core photographs, that the layers in the Marlboro clay cores could be artifacts of drilling disturbance, so-called biscuiting, wherein the formation is fractured into layers or biscuits and drilling mud is injected in between the layers. (We now prefer the term core discing following Kidd, 1978.) Here we report new observations on the cores which support that interpretation, including concentric grooves on the surfaces of the core discs caused by spinning in the bit, micro-fracturing at their edges, and injected drilling mud. We re-interpret the limited outcrop evidence as showing joints rather than sedimentary layers. We argue that foraminifer concentrations in the sediments are far too high for the layers to have been annually deposited in turbid waters at depths of 40–70 m, indicating that the onset of the CIE in the Marlboro clay likely took on the order of millennia, not years (Zeebe et al., 2014). Re-coring of Millville aimed at minimizing drilling disturbance to allow a higher-resolution study of the carbon isotope excursion is highly desirable.


2017 ◽  
Vol 46 ◽  
pp. 114-123 ◽  
Author(s):  
Qinghai Zhang ◽  
Ines Wendler ◽  
Xiaoxia Xu ◽  
Helmut Willems ◽  
Lin Ding

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