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It also lasts much longer than diazepam does, in terms of therapeutic anxiolysis, despite kpin's misleadingly shorter half life.

Dating direct events

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These younger guys are both curious and excited about dating a woman who, is not ashamed of what she wants sexually, unlike the younger girls of his own age who are often confused about just about everything, including their romantic and sexual desires.

That relationship between a younger guy and an older woman is likely to be supercharged by a combination of the younger man’s peak sex drive and the older woman’s confidence, experience and her own sex drive.

The former determines the strength of the Atlantic Ocean circulation via altering the northern hemisphere westerly winds, gulf stream, and sea-ice systems.

The latter modulates atmospheric inter-basin freshwater transport across Central America, which changes the freshwater budget in the North Atlantic and thus the circulation.

There are some other compelling reasons for why older women are more attractive to younger guys.

And of course, it’s not a secret that women in their thirties and forties have a much higher sex driver than the ones in their twenties.

This allows for the reconstruction of an older Greenland record through the derivation of the nearly million-year-long Antarctic ice core record.

In the Northern Hemisphere, they take the form of rapid warming episodes, typically in a matter of decades, each followed by gradual cooling over a longer period.

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This warmer water results in melting of Antarctic ice, thereby reducing density stratification and the strength of the Antarctic Bottom Water current (AABW).However the older parts of the GISP2 core do not show this regularity, nor do the same events in the GRIP core.This may be because the first 50 kyr of the GISP2 core are most accurately dated, by layer counting.The comparable climate cyclicity during the Holocene is referred to as Bond events.The best evidence for Dansgaard–Oeschger events remains in the Greenland ice cores, which only go back to the end of the last interglacial, the Eemian interglacial.They further suggest the existence of a window of AMOC bistability ('sweet spot' for abrupt climate changes) associated with ice volume and atmospheric CO2, accounting for the occurrences of D-O type events under intermediate glacial conditions in the late Pleistocene.