Results 111 to 120 of about 2,815 (172)

Late Cretaceous Paleoceanographic Evolution and the Onset of Cooling in the Santonian at Southern High Latitudes (IODP Site U1513, SE Indian Ocean). [PDF]

Paleoceanogr Paleoclimatol, 2022
Petrizzo MR, MacLeod KG, Watkins DK, Wolfgring E, Huber BT.   +4 more
europepmc   +1 more source

Pulsed volcanic sulfur emissions linked to the end-Triassic terrestrial crisis. [PDF]

Sci Adv
Fang L, Newton RJ, Zhang X, Li H, Wang G, Deng S, Wignall PB, Lu Y, Zhang C, Li M, Wu H, He T, Xian B, Shi S, Zhu L, Bottrell SH, Hesselbo SP.   +16 more
europepmc   +1 more source

A continental-scale Eurasian ice sheet 2.4 million years ago. [PDF]

Nat Commun
Wagner K, Ylä-Mella L, Margold M, Knudsen MF, Sørensen AL, Larsen NK, Anderson RS, Eriksen BL, Olsen J, Andersen JL, Sláma J, Jansen JD.   +11 more
europepmc   +1 more source

The Rising of Paleontology in China: A Century-Long Road. [PDF]

Biology (Basel), 2022
Zhou Z.
europepmc   +1 more source

Timing and dynamics of Late Wolstonian Substage 'Moreton Stadial' (MIS 6) glaciation in the English West Midlands, UK. [PDF]

R Soc Open Sci, 2022
Gibson SM, Bateman MD, Murton JB, Barrows TT, Fifield LK, Gibbard PL.   +5 more
europepmc   +1 more source

Belemnites of the family Belemnitellidae Pavlow, 1914 from the Late Cretaceous Maastrichtian stage in the Northern Hemisphere. [PDF]

Geol Mijnb
Keutgen N, Remin Z.
europepmc   +1 more source

Regional postdeforestation weathering feedback drove diachronous C-S cycle perturbations during the end-Permian crisis. [PDF]

Proc Natl Acad Sci U S A
Chen J, Lu B, Du L, Lin M, Shen SZ, Montañez IP, Feng Z.   +6 more
europepmc   +1 more source

Dynamic redox-promoted iron and nutrient cycling drove graptolite evolution across the Ordovician-Silurian transition. [PDF]

Sci Adv
Qiu Z, Zou C, Zhang J, Dong A, Kong W, Xiong Y, Wignall PB, Li M, Wang Z, Zhu X, Poulton SW.   +10 more
europepmc   +1 more source

Planktic foraminiferaí quantitative study across the Eocene/Oligocene boundary stratotype at Massignano (Apennines, Italy)

, 1992
The quantitative study of the planktic Foraminifera from the Eocene/Oligocene boundary stratotype at Massignano (Apennines, Italy) has been accomplished for the first time, This study allow us to establish the fauna/ changes in the assemblages, showing a
Molina, Eustoquio, Gonzalvo Ballobar, C.
core  

Global weirding at mass extinction horizons. [PDF]

Natl Sci Rev
Retallack GJ.
europepmc   +1 more source