• Tidak ada hasil yang ditemukan

Directory UMM :Data Elmu:jurnal:O:Organic Geochemistry:Vol31.Issue2-3.Feb2000:

N/A
N/A
Protected

Academic year: 2017

Membagikan "Directory UMM :Data Elmu:jurnal:O:Organic Geochemistry:Vol31.Issue2-3.Feb2000:"

Copied!
1
0
0

Teks penuh

(1)

Addendum

Addendum to ``The nature and fate of natural resins in the

geosphere. IX

1

structure and maturation similarities of

soluble and insoluble polylabdonoids isolated from Tertiary

Class I resinites''

$

[Organic Geochemistry, 30 (1999) 635±650]

David J. Cli€ord

a, b,

*, Patrick G. Hatcher

b

, Robert E. Botto

a

, John V.

Muntean

a

, Ken B. Anderson

a,

*

aChemistry Division, Argonne National Laboratory, 9700 S. Cass Avenue, Argonne, IL 60439, USA bFuel Science Program, The Pennsylvannia State University, University Park, PA 16802, USA

The authors of the above paper would like to add the following acknowledgement to their paper:

This work was performed under the auspices of the Oce of Basic Energy Sciences, Division of Chemical Sciences,

US Department of Energy, under contract number W-31-109-ENG-38.

0146-6380/00/$ - see front matter#2000 Elsevier Science Ltd. All rights reserved. P I I : S 0 1 4 6 - 6 3 8 0 ( 9 9 ) 0 0 1 4 4 - 8

Organic Geochemistry 31 (2000) 243

www.elsevier.nl/locate/orggeochem

$ PII of original article: S0146-6380(99)00018-2

* Corresponding authors. The Energy Institute, 209 Academic Projects, University Park, PA 16802, USA. Tel.: +1-814-865-3523; fax: +1-814-865-3573.

Referensi

Dokumen terkait

Recent marine sediments from two cores, collected on the continental slope of the Nansha Sea, China, have been analyzed for organic matter content, n -alkane and

The committee members unanimously agreed that all of them had made signi®cant scienti®c contributions to organic geochemistry to qualify for the Award.. However, only one could

di€erences in the relative proportion of taxa determined from the macrofossil record correlating with climatic change (Barber et al. , 1994); (ii) humi®cation of the plant

The detection of high amounts of 5,6-epoxy-24-ethylcholestan-3 b -ol (52 ng/g dry sediment at 3.5 cm depth), (resulting probably from the oxidation of 24-ethylcholest-5-en-3 b -ol

In their review of molecular fossils in Proterozoic sediments and oils, Summons and Walter (1990) show that homo- logous families of MMAs are common in sediments since 1.6 By in

These changes in lignin monomer yield, due to the brown-rot, suggest side chain alteration at a level sucient to decrease the G4 yields, such as hydro- lysis or oxidation of side

Australian Petroleum CRC/Centre for Petroleum and Environmental Organic Geochemistry, School of Applied Chemistry, Curtin University of Technology, GPO Box U1987, Perth, WA

Mass spectra for iso -15:0 fatty acid methyl ester in the Long Island Sound bulk sediment, incubated sediment (t=0 days), and incubated sediment ( t =5 days).. The occurrence of the