scholarly journals Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum

2021 ◽  
Vol 7 (42) ◽  
Author(s):  
Philip A. E. Pogge von Strandmann ◽  
Morgan T. Jones ◽  
A. Joshua West ◽  
Melissa J. Murphy ◽  
Ella W. Stokke ◽  
...  
2017 ◽  
Vol 91 (1) ◽  
pp. 363-364
Author(s):  
Licheng WANG ◽  
Chenglin LIU ◽  
Chunlian WANG ◽  
Haiming XU ◽  
Yongming ZHANG

Geology ◽  
2000 ◽  
Vol 28 (6) ◽  
pp. 507-510 ◽  
Author(s):  
Paul B. Tomascak ◽  
Jeffrey G. Ryan ◽  
Marc J. Defant

Elements ◽  
2020 ◽  
Vol 16 (4) ◽  
pp. 253-258 ◽  
Author(s):  
Philip A.E. Pogge von Strandmann ◽  
Simone A. Kasemann ◽  
Josh B. Wimpenny

Lithium and its isotopes can provide information on continental silicate weathering, which is the primary natural drawdown process of atmospheric CO2 and a major control on climate. Lithium isotopes themselves can help our understanding of weathering, via globally important processes such as clay formation and cation retention. Both these processes occur as part of weathering in modern surface environments, such as rivers, soil pore waters, and groundwaters, but Li isotopes can also be used to track weathering changes across major climate-change events. Lithium isotope evidence from several past climatic warming and cooling episodes shows that weathering processes respond rapidly to changes in temperature, meaning that weathering is capable of bringing climate back under control within a few tens of thousands of years.


Nature ◽  
2006 ◽  
Vol 443 (7111) ◽  
pp. 565-568 ◽  
Author(s):  
Tim Elliott ◽  
Alex Thomas ◽  
Alistair Jeffcoate ◽  
Yaoling Niu

2015 ◽  
Vol 432 ◽  
pp. 210-222 ◽  
Author(s):  
Maria Lechler ◽  
Philip A.E. Pogge von Strandmann ◽  
Hugh C. Jenkyns ◽  
Giacomo Prosser ◽  
Mariano Parente

Geology ◽  
2000 ◽  
Vol 28 (6) ◽  
pp. 507 ◽  
Author(s):  
Paul B. Tomascak ◽  
Jeffrey G. Ryan ◽  
Marc J. Defant

2013 ◽  
Vol 6 (8) ◽  
pp. 668-672 ◽  
Author(s):  
Philip A. E. Pogge von Strandmann ◽  
Hugh C. Jenkyns ◽  
Richard G. Woodfine

2019 ◽  
pp. 155-161 ◽  
Author(s):  
Ivan Beltran

Environmental temperature has fitness consequences on ectotherm development, ecology and behaviour. Amphibians are especially vulnerable because thermoregulation often trades with appropriate water balance. Although substantial research has evaluated the effect of temperature in amphibian locomotion and physiological limits, there is little information about amphibians living under extreme temperature conditions. Leptodactylus lithonaetes is a frog allegedly specialised to forage and breed on dark granitic outcrops and associated puddles, which reach environmental temperatures well above 40 ˚C. Adults can select thermally favourable microhabitats during the day while tadpoles are constrained to rock puddles and associated temperature fluctuations; we thus established microhabitat temperatures and tested whether the critical thermal maximum (CTmax) of L. lithonaetes is higher in tadpoles compared to adults. In addition, we evaluated the effect of water temperature on locomotor performance of tadpoles. Contrary to our expectations, puddle temperatures were comparable and even lower than those temperatures measured in the microhabitats used by adults in the daytime. Nonetheless, the CTmax was 42.3 ˚C for tadpoles and 39.7 ˚C for adults. Regarding locomotor performance, maximum speed and maximum distance travelled by tadpoles peaked around 34 ˚C, approximately 1 ˚C below the maximum puddle temperatures registered in the puddles. In conclusion, L. lithonaetes tadpoles have a higher CTmax compared to adults, suggesting a longer exposure to extreme temperatures that lead to maintain their physiological performance at high temperatures. We suggest that these conditions are adaptations to face the strong selection forces driven by this granitic habitat.


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