Syntheses of 6,7‐benzotropolone by using ring‐closing metathesis variants obviating a strongly acidic hydrolysis thereafter

Abstract: A Wittig reaction of 3-hydroxyphtalide (11) gave ortho-styrene-2-carboxylic acid (12). Its Weinreb amide 13 acylated heterosubstituted methyllithiums. This led to aryl “methyl” ketones whose sp3-carbon was substituted by Cl+OMe (in 14 a), 2×Cl (in 14 b), OtBu (in 17 a), SPh (in 17 b) or SO2Ph (in 17 c). The enolates of these ketones were C-allylated. This furnished the benzene-fused nona-1,8-dienones 7 a–b and 9 a–c, respectively. Ring-closing metatheses provided the corresponding benzocycloheptadienones 8 a-b and 10 a–c. Their ketone moieties were α,α-disubstituted (in 8 a–b) or α-monosubstituted (in 10 a–c). Each substitution pattern allowed to generate the hydroxyenone motif of the corresponding benzocycloheptatrienone—or 6,7-benzotropolone—6 a: The MeO- and PhS-containing benzocycloheptadienone 8 a gave 6,7-benzotropolone methyl ether (15) by sulfoxide formation and pyrolysis; 15 was demethylated with BCl3. The same intermediate resulted from the dichlorobenzocycloheptadienone 8 b and NaOMe. The benzocycloheptadienone 10 a was de(tert-butylated) with formic acid; a subsequent Pfitzner-Moffatt oxidation completed 6,7-benzotropolone (6 a) once more. The PhS-containing benzocycloheptadienone 10 b was α-acetoxylated with Pb(OAc)4; the resulting O,S-acetal gave 6,7-benzotropolone (6 a) by hydrolysis. The PhSO2-containing substrate 10 c was deprotonated whereupon an oxidation with Me3Si−O−O−SiMe3 gave 6,7-benzotropolone (6 a)

Location
Deutsche Nationalbibliothek Frankfurt am Main
Extent
Online-Ressource
Language
Englisch
Notes
European journal of organic chemistry. - 2022, 17 (2022) , e202101070, ISSN: 1099-0690

Event
Veröffentlichung
(where)
Freiburg
(who)
Universität
(when)
2022
Creator
Koblischek, Philip
Brückner, Reinhard

DOI
10.1002/ejoc.202101070
URN
urn:nbn:de:bsz:25-freidok-2266559
Rights
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Last update
25.03.2025, 1:51 PM CET

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Time of origin

  • 2022

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