We confirm the presence of Taconian eclogite in northwest Connecticut.
The P–T path is characterized by a post-peak-T pressure increase of > 5 kbar.
The protoliths were likely rifting-related mafic dikes that intruded in the Early Cambrian.
A new U–Pb zircon age of 456 ± 4.6 Ma (2σ) dates the timing of high-pressure metamorphism.
Taconic metamorphism took place ~ 10 Myr later in Connecticut than in Newfoundland.