| 008 |
|
150727n^^^^^^^^xx^||||^o^^^^^|||^u^eng^d |
| 245 |
00 |
|a Stop-and-go deglaciation |h [electronic resource] |y English. |
| 260 |
|
|a [S.l.] : |b Macmillan Publishers Limited, |c 2012-09. |
| 490 |
|
|a Nature Geoscience Volume 5 |y English. |
| 506 |
|
|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
| 520 |
3 |
|a Only when climate records at centennial to
millennial scales became available did the
complexity of glacial terminations become
apparent. Early low-resolution palaeoclimate
reconstructions suggested a rapid and
relentless meltdown. But at a closer look,
an interhemispheric asynchrony emerged.
Warming began in Antarctica around
18,000 years ago, which was interrupted
by an abrupt reversal about 14,500 years
ago. However, this southern cooling was
countered by warming in the Northern
Hemisphere until it too was interrupted
by 1,000 years of cooling. Full interglacial
conditions in both hemispheres were only
reached after 11,700 years ago. |
| 533 |
|
|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
| 773 |
0 |
|t Stop-and-go deglaciation |
| 852 |
|
|a dpSobek |c Sea Level Rise |
| 856 |
40 |
|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15062106/00001 |y Click here for full text |
| 856 |
42 |
|3 FULL TEXT- Stop-and-go deglaciation |u https://www.nature.com/articles/ngeo1574 |y Stop-and-go deglaciation |
| 992 |
04 |
|a http://dpanther.fiu.edu/sobek/content/FI/15/06/21/06/00001/FI15062106_thm.jpg |
