Boreal peatland water table depth and carbon accumulation during the Holocene thermal maximum, Roman Warm Period, and Medieval Climate Anomaly
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- 作者：James R. Holmquista ; HolmquistJ@si.edu" class="auth_mail" title="E-mail the corresponding author ; Robert K. Boothb ; Glen M. MacDonaldc
- 关键词：14C ; Radiocarbon ; C ; carbon ; HBL ; Hudson Bay Lowland ; HTM ; Holocene Thermal Maximum ; JBL ; James Bay Lowland ; LARCA ; Long-term apparent rate of carbon accumulation ; LIA ; Little Ice Age ; MAP ; Mean Annual Precipitation ; MAT ; Meat Annual Temperature ; MCA ; Medieval Climate Anomaly ; NAO ; North Atlantic Oscillation ; RWP ; Roman Warm Period ; SST ; Sea Surface Temperatures ; TA ; Testate Amoebae ; TJJA ; Average June ; July ; August Temperature ; WTD ; Water Table Depth ; yrBP ; years before AD 1950
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：15 February 2016
- 年：2016
- 卷：444
- 期：Complete
- 页码：15-27
- 全文大小：6616 K
文摘
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Testate amoebae used to reconstruct peatland water table depth in Boreal Ontario
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HTM moisture approached, but did not exceed, modern levels at 4600 yrBP.
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MCA pluvials are geographically similar to modern La Niña precipitation anomalies.
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Post-2550 yrBP moist conditions may have increased LARCA regionally.