New age constraints on the Lower Jurassic Pliensbachian-Toarcian Boundary at Chacay Melehue (Neuquen Basin, Argentina)

被引:25
|
作者
Al-Suwaidi, Aisha H. [1 ]
Ruhl, Micha [2 ]
Jenkyns, Hugh C. [3 ]
Damborenea, Susana E. [4 ]
Mancenido, Miguel O. [4 ]
Condon, Daniel J. [5 ]
Angelozzi, Gladys N. [6 ]
Kamo, Sandra L. [7 ]
Storm, Marisa [8 ]
Riccardi, Alberto C. [4 ]
Hesselbo, Stephen P. [9 ,10 ]
机构
[1] Khalifa Univ Sci & Technol, Dept Earth Sci, POB 12333, Abu Dhabi, U Arab Emirates
[2] Univ Dublin, Trinity Coll Dublin, Dept Geol, Dublin 2, Ireland
[3] Univ Oxford, Dept Earth Sci, South Parks Rd, Oxford OX1 3AN, England
[4] Univ Nacl La Plata, Fac Ciencias Nat & Museo, CONICET, Div Paleozool Invertebrados, Paseo Bosque S-N, RA-1900 La Plata, Argentina
[5] British Geol Survey, Keyworth NG12 5GG, Notts, England
[6] YPF Tecnol SA, Area Geociencias, Lab Bioestratig, Baradero S-N, RA-1925 Ensenada, Argentina
[7] Univ Toronto, Dept Earth Sci, Jack Satterly Geochronol Lab, 22 Ursula Franklin St, Toronto, ON M5S 3B1, Canada
[8] Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, POB 59, NL-1790 AB Den Burg, Texel, Netherlands
[9] Univ Exeter, Camborne Sch Mines, Penryn Campus, Penryn TR10 9FE, Cornwall, England
[10] Univ Exeter, Environm & Sustainabil Inst, Penryn Campus, Penryn TR10 9FE, Cornwall, England
关键词
OCEANIC ANOXIC EVENT; CLIMATIC-BIOLOGIC EVENTS; OSMIUM ISOTOPE EVIDENCE; U-PB AGE; ANTARCTIC PENINSULA; LUSITANIAN BASIN; TEMPORAL LINK; CARBON-CYCLE; KAROO LIP; BREAK-UP;
D O I
10.1038/s41598-022-07886-x
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Pliensbachian-Toarcian boundary interval is characterized by a similar to 3 parts per thousand negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from sections in Europe, such as Peniche (Portugal) and Hawsker Bottoms, Yorkshire (UK). A new high-resolution organic-carbon isotope record, illustrating the same chemostratigraphic feature, is presented from the Southern Hemisphere Arroyo Chacay Melehue section, Chos Malal, Argentina, corroborating the global significance of this disturbance to the carbon cycle. The negative carbon-isotope excursion, mercury and organic-matter enrichment are accompanied by high-resolution ammonite and nannofossil biostratigraphy together with U-Pb CA-ID-TIMS geochronology derived from intercalated volcanic ash beds. A new age of similar to 183.73 + 0.35/- 0.50 Ma for the Pliensbachian-Toarcian boundary, and 182.77 + 0.11/- 0.15 for the tenuicostatum-serpentinum zonal boundary, is assigned based on high-precision U-Pb zircon geochronology and a Bayesian Markov chain Monte Carlo (MCMC) stratigraphic age model.
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页数:10
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