Zobrazeno 1 - 10
of 30
pro vyhledávání: '"N J Shackleton"'
Publikováno v:
A Geologic Time Scale 2004. :469-484
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7afd2f5e3a6e9564e55c9169366a1e45
https://doi.org/10.1017/cbo9780511536045.026
https://doi.org/10.1017/cbo9780511536045.026
Publikováno v:
Paleoceanography. 16:405-423
High-resolution planktonic foraminiferal and oxygen isotope records are presented from a Mediterranean deep marine succession, dated astronomically between 12.12 and 9.78 Ma. Planktonic and benthic oxygen isotope records are punctuated by two episode
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e6567cf397ac2b5ef672f79eee4bc0b
https://doi.org/10.1029/2000pa000509
https://doi.org/10.1029/2000pa000509
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences. 357:1815-1829
Outcrops of Cenomanian marly chalks in the Crimea (Ukraine) and SE England (UK), 2600 km apart, display conspicuous decimetrescale rhythmicity and can be correlated by using 12 biostratigraphical events. Closely spaced samples from the two sections w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d16b75fbc09224b582b444fca5f9ed39
https://doi.org/10.1098/rsta.1999.0402
https://doi.org/10.1098/rsta.1999.0402
Autor:
N. J. Shackleton
Publikováno v:
The Carbon Cycle and Atmospheric CO2: Natural Variations Archean to Present
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d0b08975f8ff017e90a45b8a60a825e
https://doi.org/10.1029/gm032p0412
https://doi.org/10.1029/gm032p0412
Autor:
Maureen E. Raymo, Cor G. Langereis, Frederik J Hilgen, Isabella Raffi, William A. Berggren, Dennis V. Kent, N. J. Shackleton, J. D. Obradovich
Publikováno v:
Geological Society of America Bulletin. 107:1272-1287
We present an integrated geochronology for late Neogene time (Pliocene, Pleistocene, and Holocene Epochs) based on an analysis of data from stable isotopes, magnetostratigraphy, radiochronology, and calcareous plankton biostratigraphy. Discrepancies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eae04df21793d245d912bcb831e30bcf
https://doi.org/10.1130/0016-7606(1995)107<1272:lncnpi>2.3.co
https://doi.org/10.1130/0016-7606(1995)107<1272:lncnpi>2.3.co
Autor:
N. J. Shackleton, Lisa Tauxe
Publikováno v:
Geophysical Journal International. 117:769-782
SUMMARY Rock magnetic, palaeomagnetic and oxygen isotopic results are presented from core RNDB 75p, which was recovered from the Ontong-Java Plateau (OJP). A high degree of uniformity in magnetic properties characterized by relatively small changes i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a5ae0decc7e89b9c3200b6478f312e5
https://doi.org/10.1111/j.1365-246x.1994.tb02469.x
https://doi.org/10.1111/j.1365-246x.1994.tb02469.x
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences. 341:225-233
Sedimentary facies alone provide equivocal, and qualitative, evidence about Mesozoic climates and climate changes. The most climatically informative sediments are laterites, evaporites and aeolianites. Tills would also be unequivocal where present. A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa1b3c57b52b57826805077a58cea414
https://doi.org/10.1098/rstb.1993.0107
https://doi.org/10.1098/rstb.1993.0107
Autor:
J. Imbrie, N. J. Shackleton
Publikováno v:
Climatic Change. 16:217-230
We have examined the climatic variance in a series of deep-water oxygen-isotope records which range in length from 0.3 to 130 million years and have temporal resolutions between one thousand and 10 million years. These variations in δ 18O are interp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15db5cf41fd82b1aad5c8a85ed4b8642
https://doi.org/10.1007/bf00134658
https://doi.org/10.1007/bf00134658