Tungsten isotopic constraints on the age and origin of chondrules.

Abstract:

:Chondrules may have played a critical role in the earliest stages of planet formation by mediating the accumulation of dust into planetesimals. However, the origin of chondrules and their significance for planetesimal accretion remain enigmatic. Here, we show that chondrules and matrix in the carbonaceous chondrite Allende have complementary (183)W anomalies resulting from the uneven distribution of presolar, stellar-derived dust. These data refute an origin of chondrules in protoplanetary collisions and, instead, indicate that chondrules and matrix formed together from a common reservoir of solar nebula dust. Because bulk Allende exhibits no (183)W anomaly, chondrules and matrix must have accreted rapidly to their parent body, implying that the majority of chondrules from a given chondrite group formed in a narrow time interval. Based on Hf-W chronometry on Allende chondrules and matrix, this event occurred ∼2 million years after formation of the first solids, about coeval to chondrule formation in ordinary chondrites.

authors

Budde G,Kleine T,Kruijer TS,Burkhardt C,Metzler K

doi

10.1073/pnas.1524980113

subject

Has Abstract

pub_date

2016-03-15 00:00:00

pages

2886-91

issue

11

eissn

0027-8424

issn

1091-6490

pii

1524980113

journal_volume

113

pub_type

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