Tree ring effects and ice core acidities clarify the volcanic record of the first millennium

被引:41
作者
Baillie, M. G. L. [1 ]
McAneney, J. [1 ]
机构
[1] Queens Univ Belfast, Sch Geog Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland
关键词
ELDGJA ERUPTION; CLIMATIC IMPACT; GREENLAND; VARIABILITY; CHINA; ASH;
D O I
10.5194/cp-11-105-2015
中图分类号
P [天文学、地球科学];
学科分类号
070403 [天体物理学];
摘要
In 2012 Plummer et al., in presenting the volcanic chronology of the Antarctic Law Dome ice core, chose to list connections to acid layers in other ice cores and also possible chronological coincidences between ice acid dates and the precise dates of frost damage, and/or reduced growth in North American bristlecone pines. We disagree with the chronological links indicated by Plummer et al. for the period before AD 700, and in this paper we show that a case can be made that better linkages between ice acid and tree ring effects occur for this period if the ice chronologies are systematically moved forward by around 7 years, consistent with a hypothesis published by Baillie in 2008. In the paper we seek to explore the proposition that frost damage rings in North American bristlecone pines are a very useful indicator of the dates of certain large explosive volcanic eruptions; the dating of major eruptions being critical for any clear understanding of volcanic forcing. This paper cannot prove that there is an error in the Greenland Ice Core Chronology 2005 (GICC05), and in equivalent ice chronologies from the Antarctic, however, it does provide a coherent argument for an apparent ice dating offset. If the suggested offset were to prove correct it would be necessary to locate where the error occurs in the ice chronologies and in this regard the dating of the increasingly controversial Icelandic Eldgja eruption in the AD 930s, and the China/Korean Millennium eruption which occurs some 7 years after Eldgja, may well be critical. In addition, if the offset were to be substantiated it would have implications for the alleged identification of tephra at 429.3m in the Greenland GRIP core, currently attributed to the Italian volcano Vesuvius and used as a critical zero error point in the GICC05 chronology.
引用
收藏
页码:105 / 114
页数:10
相关论文
共 45 条
[1]
Arjava A., 2005, DOP, V59, P73, DOI DOI 10.2307/4128751
[2]
Volcanoes, ice-cores and tree-rings: one story or two? [J].
Baillie, M. G. L. .
ANTIQUITY, 2010, 84 (323) :202-215
[3]
Proposed re-dating of the European ice core chronology by seven years prior to the 7th century AD [J].
Baillie, M. G. L. .
GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (15)
[4]
Baillie M. G. L., 1994, Holocene, V4, P212, DOI 10.1177/095968369400400211
[5]
Greenland ice core evidence of the 79 AD Vesuvius eruption [J].
Barbante, C. ;
Kehrwald, N. M. ;
Marianelli, P. ;
Vinther, B. M. ;
Steffensen, J. P. ;
Cozzi, G. ;
Hammer, C. U. ;
Clausen, H. B. ;
Siggaard-Andersen, M. -L. .
CLIMATE OF THE PAST, 2013, 9 (03) :1221-1232
[6]
Barras C., 2014, NEW SCIENTIST, V221, P34
[7]
BONINSEGNA J A, 1985, Tree-Ring Bulletin, V45, P37
[8]
Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years [J].
Briffa, KR ;
Jones, PD ;
Schweingruber, FH ;
Osborn, TJ .
NATURE, 1998, 393 (6684) :450-455
[9]
A comparison of the volcanic records over the past 4000 years from the Greenland Ice Core Project and Dye 3 Greenland Ice Cores [J].
Clausen, HB ;
Hammer, CU ;
Hvidberg, CS ;
DahlJensen, D ;
Steffensen, JP ;
Kipfstuhl, J ;
Legrand, M .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1997, 102 (C12) :26707-26723
[10]
Volcanic cooling signal in tree ring temperature records for the past millennium [J].
D'Arrigo, Rosanne ;
Wilson, Rob ;
Anchukaitis, Kevin J. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2013, 118 (16) :9000-9010