This FLIP «fingerprint» was found to be restricted to
the Pliocene warm intervals and was absent from the overlying younger sediments.
Not exact matches
DeConto and Pollard's study was motivated by reconstructions of sea level rise during past
warm periods including the previous inter-glacial (around 125,000 years ago) and earlier
warm intervals like the
Pliocene (around 3 million years ago).
The new results, published in Nature Geoscience, contradict those previous studies and indicate that tropical sea surface temperatures were
warmer during the early - to - mid
Pliocene, an
interval spanning about 5 to 3 million years ago.
Its key finding is that during the
Pliocene there occurred a series of long,
warm intervals during which parts of the East Antarctic Ice - Sheet margin retreated hundreds of kilometres inland.
The most recent
interval in which sustained global temperatures exceeded those of today was during the
Pliocene epoch (2.6 — 5.3 Ma), when global surface temperatures were between 2 and 3 °C
warmer than present (Dowsett, 2007).
The
Pliocene is a paradox when compared to other Cenozoic
warm intervals because global mean temperatures were 2 — 3 °C
warmer than present (Dowsett, 2007), despite levels of atmospheric CO2 that were only slightly higher than preindustrial levels (Fedorov et al., 2006).
During the
warm intervals of the middle
Pliocene (3.3 to 3.0 million years ago), when there is medium confidence that global mean surface temperatures were 2 °C to 3.5 °C
warmer than for pre-industrial climate and CO2 levels were between 250 and 450 ppm, sedimentary records suggest periodic deglaciation of West Antarctica and parts of East Antarctica.