Characterisation of early Archaean chemical sediments by trace element signatures

被引:712
作者
Bolhar, R [1 ]
Kamber, BS
Moorbath, S
Fedo, CM
Whitehouse, MJ
机构
[1] ACQUIRE, Brisbane, Qld 4072, Australia
[2] Univ Oxford, Dept Earth Sci, Oxford OX1 3PR, England
[3] George Washington Univ, Dept Earth & Environm Sci, Washington, DC 20052 USA
[4] Swedish Museum Nat Hist, Lab Isotope Geol, SE-10405 Stockholm, Sweden
关键词
Archaean; banded iron formation; Isua Greenstone Belt; chemical sediments; metasomatism; REE plus Y; seawater composition;
D O I
10.1016/j.epsl.2004.02.016
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Rare earth element (REE) plus yttrium (Y) patterns of modem seawater have characteristic features that can be used as chemical fingerprints. Reliable proxies for marine REE + Y chemistry have been demonstrated from a large geological time span, including Archaean banded iron formation (BIF), stromatolitic limestone, Phanerozoic reef carbonate and Holocene microbialite. Here we present new REE + Y data for two distinct suites of early Archaean (ca. 3.7-3.8 Ga) metamorphosed rocks from southern West Greenland, whose interrelationships, if any, have been much debated in recent literature. The first suite comprises mangetite-quartz BIF, magnetite-carbonate BIF and banded magnetite-rich quartz rock, mostly from the Isua Greenstone Belt (IGB). The REE + Y patterns, particularly diagnostic anomalies (Ce/Ce*, Pr/Pr*), are closely related to those of published seawater proxies. The second suite includes banded quartz-pyroxene-amphibole +/- garnet rocks with minor magnetite from the so-called Akilia Association enclaves (in early Archaean granitoid gneisses) of the coastal region, some 150 km southwest of the IGB. Rocks of this type from one much publicised and highly debated locality (the island of Akilia) have been identified by some workers [Nature 384 (1996) 55; Geochim. Cosmochim. Acta 61 (1997) 2475] as BIF-facies, and their C-13-depleted signature in trace graphite interpreted as a proxy for earliest life on Earth. However, REE + Y patterns of the Akilia Association suite (except for one probably genuine magnetite-rich BIF from Ugpik) are inconsistent with a seawater origin. We agree with published geological and geochemical (including REE) work [Science 296 (2002) 1448] that most of the analysed Akilia rocks are not chemical sediments, and that C-isotopes in such rocks therefore cannot be used as biological proxies. Application of the REE + Y discriminant for the above two rock suites has been facilitated in this study by the use of MC-ICP technique which yields a more complete and precise REE + Y spectrum than was available in many previous studies. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:43 / 60
页数:18
相关论文
共 62 条
[11]  
BOLHAR R, UNPUB GEOCHIMICA COS
[12]   Questioning the evidence for Earth's oldest fossils [J].
Brasier, MD ;
Green, OR ;
Jephcoat, AP ;
Kleppe, AK ;
Van Kranendonk, MJ ;
Lindsay, JF ;
Steele, A ;
Grassineau, NV .
NATURE, 2002, 416 (6876) :76-81
[13]   COMPARATIVE YTTRIUM AND RARE-EARTH ELEMENT CHEMISTRIES IN SEAWATER [J].
BYRNE, RH ;
LEE, JH .
MARINE CHEMISTRY, 1993, 44 (2-4) :121-130
[14]   THE EUROPIUM ANOMALIES IN BANDED IRON FORMATIONS AND THE THERMAL HISTORY OF THE OCEANIC-CRUST [J].
DANIELSON, A ;
MOLLER, P ;
DULSKI, P .
CHEMICAL GEOLOGY, 1992, 97 (1-2) :89-100
[15]   RARE-EARTH ELEMENTS IN THE PACIFIC AND ATLANTIC OCEANS [J].
DEBAAR, HJW ;
BACON, MP ;
BREWER, PG ;
BRULAND, KW .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1985, 49 (09) :1943-1959
[16]  
DEBAAR HJW, 1991, EUR J SOL STATE INOR, V28, P357
[17]   ANOMALIES IN RARE-EARTH DISTRIBUTIONS IN SEAWATER - GD AND TB [J].
DEBAAR, HJW ;
BREWER, PG ;
BACON, MP .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1985, 49 (09) :1961-1969
[18]   THE CHEMICAL EVOLUTION OF PRECAMBRIAN SEAWATER - EVIDENCE FROM REES IN BANDED IRON FORMATIONS [J].
DERRY, LA ;
JACOBSEN, SB .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1990, 54 (11) :2965-2977
[19]   Reference materials for geochemical studies: New analytical data by ICP-MS and critical discussion of reference values [J].
Dulski, P .
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS, 2001, 25 (01) :87-125
[20]   A simple method for the precise determination of >=40 trace elements in geological samples by ICPMS using enriched isotope internal standardisation [J].
Eggins, SM ;
Woodhead, JD ;
Kinsley, LPJ ;
Mortimer, GE ;
Sylvester, P ;
McCulloch, MT ;
Hergt, JM ;
Handler, MR .
CHEMICAL GEOLOGY, 1997, 134 (04) :311-326