At least 28 rhyolitic lava flows, domes, and tuffs erupted within Yellowstone caldera following its formation 631 ka. Understanding the timing of intracaldera eruptions is essential for characterizing natural hazards posed by Yellowstone volcano. We present Ar-40/Ar-39 eruption ages for the Mallard Lake Member and Central Plateau Member of the Plateau Rhyolite, which comprise products from 22 eruptions spanning similar to 160 to similar to 70 ka. These eruptions occurred along two linear vent zones within Yellowstone caldera that appear to be extensions of major extracaldera normal faults. Eruptions took place in five brief clusters with group mean ages of 160.3 +/- 1.0 ka (2 sigma), 149.8 +/- 4.0 ka, 111.4 +/- 0.9 ka, 104.1 +/- 0.8 ka, and 70.8 +/- 0.7 ka. All mapped products within each informal group have indistinguishable Ar-40/Ar-39 eruption ages implying brief eruption durations. Eruption products of each group are spatially clustered, with only one of the two linear vent zones being active during an eruption group. Using the oldest group (160 ka), we apply paleomagnetic and geochemical analyses to investigate the duration of these eruption groups and their pre-eruptive magma reservoir configuration. Paleomagnetic analyses suggest that the nine rhyolite eruptions similar to 160 ka spanned 400 years or less. Glass and sanidine compositions of each rhyolite are nearly identical, which is consistent with pre-eruptive storage of a large (similar to 130 km(3)), interconnected melt body within Yellowstone volcano's crystal-rich magma reservoir. These characteristics differ from intracaldera eruptions that vented near the caldera's inner ring fracture system, which tend to be compositionally disparate with less temporal clustering. These insights inform hazard mitigation scenarios.
