Beryllium-10 in deep-sea sediments: a tracer for the Earth's magnetic field intensity during the last 200,000 years

被引：38

作者：

Christl, M ^{[1
]}

Strobl, C ^{[1
]}

Mangini, A ^{[1
]}

机构：

[1] Univ Heidelberg, Hiedelberg Acad Sci, Inst Environm Phys, D-69120 Heidelberg, Germany

来源：

QUATERNARY SCIENCE REVIEWS | 2003年 / 22卷 / 5-7期

关键词：

D O I：

10.1016/S0277-3791(02)00195-6

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

We present a new approach for the reconstruction of the Earth's magnetic field intensity during the last 200,000 years based on Be-10 in deep-sea sediments. A simple box model that is able to describe boundary scavenging of Be-10 in the ocean is used to study the sensitivity of Be-10 to changes of water circulation and/or varying particle rain rates. The model is applied to separate transport and production signal in single Be-10 records. Vertical sediment accumulation rates are used as input values for the model calculations. The calculated scavenging factors are applied to correct the Be-10 records for boundary scavenging. The model corrected Be-10 based paleointensity record correlates well with other records from very different archives. (C) 2002 Published by Elsevier Science Ltd.

引用

页码：725 / 739

页数：15

共 26 条

[1] THE BERYLLIUM-10 CONCENTRATION IN DEEP-SEA SEDIMENTS
GOEL, PS
KHARKAR, DP
LAL, D
NARSAPPAYA, N
PETERS, B
YATIRAJAM, V
DEEP-SEA RESEARCH, 1957, 4 (03): : 202 - 210
[2] Nature and dynamics of North African humid and dry periods during the last 200,000 years documented in the clay fraction of Eastern Mediterranean deep-sea sediments
Ehrmann, Werner
Schmiedl, Gerhard
QUATERNARY SCIENCE REVIEWS, 2021, 260
[3] Stalagmites indicate a link between Earth's magnetic field and climate during the past 200,000 years
Mangini, A
GEOCHIMICA ET COSMOCHIMICA ACTA, 2002, 66 (15A) : A480 - A480
[4] EXPLOSIVE VOLCANIC ACTIVITY IN MEDITERRANEAN OVER PAST 200,000 YR AS RECORDED IN DEEP-SEA SEDIMENTS
KELLER, J
RYAN, WBF
NINKOVICH, D
ALTHERR, R
GEOLOGICAL SOCIETY OF AMERICA BULLETIN, 1978, 89 (04) : 591 - 604
[5] Variations in solar magnetic activity during the last 200,000 years: is there a Sun-climate connection?
Sharma, M
EARTH AND PLANETARY SCIENCE LETTERS, 2002, 199 (3-4) : 459 - 472
[6] Precessional forcing of coccolithophore assemblages in the northern Arabian Sea: Implications for monsoonal dynamics during the last 200,000 years
Rogalla, U
Andruleit, H
MARINE GEOLOGY, 2005, 217 (1-2) : 31 - 48
[7] THE MICROMETEORITE FLUX TO THE EARTH, DURING THE LAST - 200,000 YEARS AS DEDUCED FROM COSMIC SPHERULE CONCENTRATION IN ANTARCTIC ICE CORES
YIOU, F
RAISBECK, GM
JEHANNO, C
METEORITICS, 1991, 26 (04): : 412 - 412
[8] A REVERSAL OF EARTHS MAGNETIC FIELD IN INTERVALS OF 1350 YEARS, INVESTIGATED BY DEEP-SEA SEDIMENTS
HEYE, D
EARTH AND PLANETARY SCIENCE LETTERS, 1970, 9 (01) : 82 - &
[9] A 200 kyr record of cosmogenic radionuclide production rate and geomagnetic field intensity from 10 Be in globally stacked deep-sea sediments
Frank, M.
Schwarz, B.
Baumann, S.
Kubik, P. W.
Earth and Planetary Science Letters, 149 (1-4):
[10] Evidence for a link between the flux of galactic cosmic rays and Earth's climate during the past 200,000 years
Christl, M
Mangini, A
Holzkämper, S
Spötl, C
JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2004, 66 (3-4) : 313 - 322

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