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Holocene North Atlantic and Arctic oceanic currents changes.

Benthic C-rich North Atlantic deepwater (NADW) contribution.

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Conclusions 1) A 2600-year climate cycle was first proposed in the late 1960s by Roger Bray based on vegetation transitions and major glacier re-advances, and linked to solar activity.

His research shows very clearly the impact of Holocene climatic change.

Winter precipitation reconstruction at Bjørnbreen glacier in Jotunheimen, southern Norway.

This has had the result that whatever is not prominently displayed in polar ice cores is considered unreal.

The lows in the Bray cycle (blue bars), correspond to periods of reduced NADW contribution.

For decades Michael Magny has been studying Holocene mid-European lake level fluctuations and their impact on prehistoric human settlements (Magny et al., 2004)."Fantastic, I'd have never joined up to online dating if it wasn't for a friend of mine who set me up on your site.I've never been a fan of writing about myself or trying to 'big' myself up......Even B5, when the world was still experiencing the fast warming that led to the HCO, shows a significant departure from the warming trend of the previous centuries.This conclusion agrees well with the other evidence shown here for the Bray climate cycle.Apparently, I wasn’t alone in my Valentine’s Day depression-induced hunt for Prince Charming.

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