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The increased use of radiocarbon analyses for archeological, paleontological, and paleoclimate research has created a demand for robust and well characterized procedural blanks. Currently, blanks are distributed ad hoc throughout the radiocarbon community in limited quantities and are depleted quickly by high throughput labs. This forces AMS facilities to regularly seek out suitable blanks from other facilities, and the switch to different blank material inhibits assessment of long term procedural blank performance. An excellent source for well-preserved radiocarbon "dead" organic material is the permafrost-rich region of unglaciated Yukon and Alaska. Extensive placer mining operations and river bluffs expose Middle Pleistocene sediments that regularly yield pristine organic material. Here, we present an assessment of laboratory precision and overall measure of performance of two processing blanks from the region. The AVR-07-PAL-37 wood and Hollis Mammoth pelvis bone collected from Alaska and Yukon, respectively. Both are independently dated to the Middle Pleistocene and have been verified by 14C-AMS to be radiocarbon "dead", with mean FmC of 0.0054 ± 0.0002 (n = 714) and 0.0031 ± 0.0002, (n = 219), respectively. Preliminary use at several AMS and stable isotope facilities in the U.S.A., Canada, United Kingdom, and China confirms that AVR-07-PAL-37 and Hollis Mammoth are suitable blanks for radiocarbon analyses. Both materials are available for wide distribution to other interested AMS labs. [ABSTRACT FROM AUTHOR]