Daniel J Condon
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Explore the profile of Daniel J Condon including associated specialties, affiliations and a list of published articles.
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10
Citations
238
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Recent Articles
1.
Olierook H, Fougerouse D, Doucet L, Liu Y, Rayner M, Danisik M, et al.
Nat Commun
. 2023 Sep;
14(1):5274.
PMID: 37726314
Argyle is the world's largest source of natural diamonds, yet one of only a few economic deposits hosted in a Paleoproterozoic orogen. The geodynamic triggers responsible for its alkaline ultramafic...
2.
Fu H, Zhang S, Condon D, Xian H
Sci Adv
. 2022 Oct;
8(41):eabo2753.
PMID: 36240274
The rate of movement of Earth's solid shell relative to its spin axis, or true polar wander, depends on variations in mantle convection and viscosity. We report paleomagnetic and geochronologic...
3.
Al-Suwaidi A, Ruhl M, Jenkyns H, Damborenea S, Mancenido M, Condon D, et al.
Sci Rep
. 2022 Mar;
12(1):4975.
PMID: 35322043
The Pliensbachian-Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from sections in Europe, such as Peniche (Portugal)...
4.
Yang C, Rooney A, Condon D, Li X, Grazhdankin D, Bowyer F, et al.
Sci Adv
. 2021 Nov;
7(45):eabi9643.
PMID: 34731004
The rise of complex macroscopic life occurred during the Ediacaran Period, an interval that witnessed large-scale disturbances to biogeochemical systems. The current Ediacaran chronostratigraphic framework is of insufficient resolution to...
5.
Warke M, Di Rocco T, Zerkle A, Lepland A, Prave A, Martin A, et al.
Proc Natl Acad Sci U S A
. 2020 Jun;
117(24):13314-13320.
PMID: 32482849
The inability to resolve the exact temporal relationship between two pivotal events in Earth history, the Paleoproterozoic Great Oxidation Event (GOE) and the first "snowball Earth" global glaciation, has precluded...
6.
Himmler T, Sahy D, Martma T, Bohrmann G, Plaza-Faverola A, Bunz S, et al.
Sci Adv
. 2019 Aug;
5(8):eaaw1450.
PMID: 31457082
The geological factors controlling gas release from Arctic deep-water gas reservoirs through seabed methane seeps are poorly constrained. This is partly due to limited data on the precise chronology of...
7.
Parry L, Boggiani P, Condon D, Garwood R, Leme J, McIlroy D, et al.
Nat Ecol Evol
. 2017 Nov;
1(10):1455-1464.
PMID: 29185521
The evolutionary events during the Ediacaran-Cambrian transition (~541 Myr ago) are unparalleled in Earth history. The fossil record suggests that most extant animal phyla appeared in a geologically brief interval,...
8.
Cremiere A, Lepland A, Chand S, Sahy D, Condon D, Noble S, et al.
Nat Commun
. 2016 May;
7:11509.
PMID: 27167635
Gas hydrates stored on continental shelves are susceptible to dissociation triggered by environmental changes. Knowledge of the timescales of gas hydrate dissociation and subsequent methane release are critical in understanding...
9.
Hiess J, Condon D, McLean N, Noble S
Science
. 2012 Mar;
335(6076):1610-4.
PMID: 22461608
The present-day (238)U/(235)U ratio has fundamental implications for uranium-lead geochronology and cosmochronology. A value of 137.88 has previously been considered invariant and has been used without uncertainty to calculate terrestrial...
10.
Love G, Grosjean E, Stalvies C, Fike D, Grotzinger J, Bradley A, et al.
Nature
. 2009 Feb;
457(7230):718-21.
PMID: 19194449
The Neoproterozoic era (1,000-542 Myr ago) was an era of climatic extremes and biological evolutionary developments culminating in the emergence of animals (Metazoa) and new ecosystems. Here we show that...