Paleorecords of the middle Holocene (MH) from the North American mid-continent can offer insights into ecological responses to pervasive drought that may accompany future climatic warming. We analyzed MH sediments from West Olaf Lake (WOL) and Steel Lake (SL) in Minnesota to examine the effects of warm͞dry climatic conditions on prairie-woodland ecosystems. Mineral composition and carbonate ␦ 18 O were used to determine climatic variations, whereas pollen assemblages, charcoal ␦ 13 C, and charcoal accumulation rates were used to reconstruct vegetation composition, C3 and C4 plant abundance, and fire. The ratio of aragonite͞calcite at WOL and ␦ 18 O at SL suggest that pronounced droughts occurred during the MH but that drought severity decreased with time. From charcoal ␦ 13 C data we estimated that the MH abundance of C4 plants averaged 50% at WOL and 43% at SL. At WOL C4 abundance was negatively correlated with aragonite͞calcite, suggesting that severe moisture deficits suppressed C4 plants in favor of weedy C3 plants (e.g., Ambrosia). As climate ameliorated C4 abundance increased (from Ϸ33 to 66%) at the expense of weedy species, enhancing fuel availability and fire occurrence. In contrast, farther east at SL where climate was cooler and wetter, C 4 abundance showed no correlation with ␦ 18 O-inferred aridity. Woody C 3 plants (e.g., Quercus) were more abundant, biomass flammability was lower, and fires were less important at SL than at WOL. Our results suggest that C 4 plants are adapted to warm͞dry climatic conditions, but not to extreme droughts, and that the fire regime is controlled by biomass-climate interactions. P ervasive drought, expected to be associated with climatic change in continental interiors, will have profound ecological, economic, and societal repercussions (1-4). Drought conditions are likely to alter ecosystem function by changing the relative abundance of plant functional groups (e.g., C 3 vs. C 4 ) in natural systems (5-7). For example, episodic droughts that occurred throughout the 20th century in the midwestern United States killed woody C 3 genera, such as Quercus (8-10), and favored better adapted C 3 and C 4 herbaceous species (9). General circulation models coupled with dynamic crop-growth models project that, in agricultural systems, such climatic conditions could significantly reduce both C 3 (e.g., wheat, Triticum aestivum L.) and C 4 (e.g., corn, Zea mays L.) cereal crop yields (11,12), resulting in billions of dollars of economic loss (13,14). Empirical evidence of the response of plant functional groups to climatic conditions characteristic of drought is therefore important for evaluating predictions of future change. However, such evidence is mostly limited to historical records (15, 16), which lack the full range of past drought variability (3), and to short-term experimental manipulations (17, 18), which lack a sufficient temporal dimension for understanding future vegetational response.During the middle Holocene (MH), Ϸ8.0-4.0 thousand years (ka) B.P. (19), the midweste...