新澳门六合彩内幕信息

The pressing concern posed by rising sea levels has created a critical need for scientists to precisely predict how quickly the oceans will rise in coming centuries. To gain insight into future ice sheet stability and sea-level rise, new research from an international team led by 新澳门六合彩内幕信息 geoscientists is drawing on evidence from past interglacial periods when Earth鈥檚 climate was warmer than today.

Using deposits in the caves of the Mediterranean island of Mallorca, known as phreatic overgrowths on speleothems, to reconstruct past sea level stands, the team was able to determine that the vertical extent of these unique deposits corresponds with the amplitude of the fluctuating water table, said author 新澳门六合彩内幕信息geosciences . That determination now is providing scientists with a way to precisely measure past sea levels.

Working with colleagues at the University of New Mexico, University of Balearic Islands and Columbia University, the researchers鈥� findings were published in In their project, the geosciences team documented the position and timing of sea level during key time intervals over the past 6.5 million years for which global mean sea-level estimates have been highly uncertain.

Their results contribute to the understanding of past warm periods to gain insight into the magnitude and frequency of sea level rise, which is critical for scientists鈥� ability to forecast and make recommendations on adapting to future global warming.

The team expanded upon their research previously published in by investigating samples between 800,000 and 6.5 million years old. Using deposits from several of the Mallorcan caves and applying numerical and statistical models to estimate the corrections for glacial isostatic adjustment and long鈥恡erm uplift, they translated the local sea level estimates into global mean sea level (GMSL).

Their results show that during key time events, such as Pliocene鈥揚leistocene Transition, when the Earth underwent a major transition from the warm climates of the Pliocene to the Pleistocene ice ages, the GMSL stood at 6.4 meters. During the beginning and the end of the Mid鈥怭leistocene Transition the sea level was at 鈭�1.1 meter and 5 meters respectively.

鈥淥verall, our results support that sea level dropped significantly after the Pliocene,鈥� said 新澳门六合彩内幕信息doctoral alum Oana Dumitru, the study鈥檚 lead author who is now a postdoc at Columbia University鈥檚 Lamont-Doherty Earth Observatory.

The authors also show that local sea level before and at the onset of the Messinian Salinity Crisis, a major geological event during which the Mediterranean Sea became partly to nearly dry of water, was at approximately 33 meters above present level. These estimates may offer starting points for assessing whether sea-level drawdown in the Western Mediterranean happened gradually or rapidly, the researchers said.

鈥淥ur estimates are important snapshots of sea level still stands, but additional sea level index points will be useful to yield more context for our results,鈥� the team wrote in their journal article. 鈥淏y providing direct estimates of sea level using POS as robust proxies, this work advances our understanding of sea level position during several past warm periods. These results therefore contribute to efforts of studying past warm periods to gain insight into the magnitude and frequency of sea level rise.鈥�

Dumitru was joined in the research by Columbia University colleague Jacqueline Austermann; Victor J. Polyak and Yemane Asmerom of the University of New Mexico; Joan J. Forn贸s, Joaquin Gin茅s and Angel Gin茅s of Universitat de les Illes Balears in Mallorca, Spain.

This research is the result of a collaborative National Science Foundation (NSF) project between the 新澳门六合彩内幕信息 and the University of New Mexico and part of the bilateral agreement between 新澳门六合彩内幕信息and Universitat de les Illes Balears and has been funded by NSF and the Spanish State Research Agency.