Abstract

Here we presented a high-resolution 5350-year pollen record from a maar annually laminated lake in East Asia (EA). Pollen record reflected the dynamics of vertical vegetation zones and temperature change. Spectral analysis on pollen percentages/concentrations of Pinus and Quercus, and a temperature proxy, revealed ~500-year quasi-periodic cold-warm fluctuations during the past 5350 years. This ~500-year cyclic climate change occurred in EA during the mid-late Holocene and even the last 150 years dominated by anthropogenic forcing. It was almost in phase with a ~500-year periodic change in solar activity and Greenland temperature change, suggesting that ~500-year small variations in solar output played a prominent role in the mid-late Holocene climate dynamics in EA, linked to high latitude climate system. Its last warm phase might terminate in the next several decades to enter another ~250-year cool phase, and thus this future centennial cyclic temperature minimum could partially slow down man-made global warming.

Highlights

  • We presented a high-resolution 5350-year pollen record from a maar annually laminated lake in East Asia (EA)

  • Spectral analysis on pollen percentages/concentrations of Pinus and Quercus, and a temperature proxy, revealed,500-year quasi-periodic cold-warm fluctuations during the past 5350 years. This,500-year cyclic climate change occurred in EA during the mid-late Holocene and even the last 150 years dominated by anthropogenic forcing

  • The climate conditions in the study region are controlled by East Asian monsoon system

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Summary

Introduction

We presented a high-resolution 5350-year pollen record from a maar annually laminated lake in East Asia (EA). Spectral analysis on pollen percentages/concentrations of Pinus and Quercus, and a temperature proxy, revealed ,500-year quasi-periodic cold-warm fluctuations during the past 5350 years This ,500-year cyclic climate change occurred in EA during the mid-late Holocene and even the last 150 years dominated by anthropogenic forcing. Observations and model simulations over recent centuries suggested that multidecadal to multicentennial cyclic change of solar activity and climate patterns (such as Pacific Decadal Oscillation, Atlantic Multidecadal Oscillation, and North Atlantic Deep Water) still existed under anthropogenic forcing and played an important role in regulating global to regional terrestrial (EA, North America, and Europe) and marine (North Atlantic and Pacific) climate change during the past centuries[9,10,11,12,13,14,15]. We discussed the mechanisms for this multicentennial climate oscillation

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