منابع مشابه
deglaciation High tide of the warm Pliocene : Implications of global sea level for Antarctic
doi: 10.1130/G32869.1 2012;40;407-410 Geology Naish, Benjamin S. Cramer, Yair Rosenthal, W. Richard Peltier and Sindia Sosdian Kenneth G. Miller, James D. Wright, James V. Browning, Andrew Kulpecz, Michelle Kominz, Tim R. deglaciation High tide of the warm Pliocene: Implications of global sea level for Antarctic Email alerting services articles cite this article to receive free e-mail alerts wh...
متن کاملCrowdsourcing in the Quaternary sea level community: insights from the Pliocene
In order to establish the ‘fingerprint’ of past sea level changes, many field measurements of paleo sea level from globally distributed locations are needed. It is because this problem requires a geographically expansive database that it becomes an ideal candidate for crowdsourcing techniques. In order to crowdsource sea level data from the Mid-Pliocene Warm Period, we developed three tools: Pl...
متن کاملLightweight Snapshots and System-level Backtracking
We propose a new system-level abstraction, the lightweight immutable execution snapshot, which combines the immutable characteristics of checkpoints with the direct integration into the virtual memory subsystem of standard mutable address spaces. The abstraction can give arbitrary x86 programs and libraries system-level support for backtracking (akin to logic programming) and the ability to man...
متن کاملCaspian Sea Level Fluctuations
In this paper the main factors that influence the Caspian Sea level rising and the probable and improbable factors are discussed in detail. A cyclical behavior of the level of the Caspian Sea according to local records was proposed. This cyclic fluctuation of the sea level is the long-term behavior of the sea so that the investigation is not restricted to a specific time interval. The statistic...
متن کاملMid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes.
Ostracode magnesium/calcium (Mg/Ca)-based bottom-water temperatures were combined with benthic foraminiferal oxygen isotopes in order to quantify the oxygen isotopic composition of seawater, and estimate continental ice volume and sea-level variability during the Mid-Pliocene warm period, ca 3.3-3.0Ma. Results indicate that, following a low stand of approximately 65m below present at marine iso...
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ژورنال
عنوان ژورنال: TheScienceBreaker
سال: 2020
ISSN: 2571-9262
DOI: 10.25250/thescbr.brk354