A 7500‐year record of fire and precipitation dynamics from Clear Pond, South Carolina, USA

ABSTRACT We analyzed a 2.38 m sediment core from Clear Pond, South Carolina, to reconstruct fire and effective moisture over the past 7500 years in a Pinus ‐ Quercus forest. Our record of macroscopic charcoal, reconstructed precipitation isotopes from δ 2 H n‐alkane analysis, and other geochemical indicators provides a high‐resolution record of the interplays between fire and effective moisture on the Atlantic Coastal Plain (ACP). Our work complements and updates an existing pollen and microscopic charcoal record from Clear Pond with additional analyses, including reconstructed effective moisture. δ 2 H n‐alkane values are indicative of soil moisture isotopic values, which are controlled by precipitation δ 2 H values and fractionation during evaporation and transpiration. Our results show that from ca. 7500–3670 cal yr bp , effective moisture was higher than modern conditions at Clear Pond, but fires were frequent. Our δ 2 H n‐alkane record of effective moisture indicates that conditions remained mesic from ca. 3670 cal yr bp until 2350 cal yr bp , but macroscopic charcoal data indicate that fires were much less frequent than before. This pattern is in opposition to several nearby records on the ACP, where much of this timespan was apparently somewhat dry with frequent fires. After ca. 2350 cal yr bp , effective moisture slightly increased, and frequent fires returned to the landscape. These conditions persisted until about ca. 860 cal yr bp , when δ 2 H‐derived effective moisture values reached their most positive values, indicating xeric conditions, and charcoal data indicate a declining importance of fire on the landscape. Over the past 7500 years at Clear Pond, there is an apparent decoupling of reconstructed paleomoisture indicators and macroscopic charcoal records, which indicates that fire is not largely controlled by climate on the ACP and that landscape burning by Native Americans may be an important control on Holocene fire regimes at Clear Pond, especially from ca. 7500–2350 cal yr bp .

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Journal
Journal of Quaternary Science
Published
2025-04-03
DOI
https://doi.org/10.1002/jqs.3711
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

A 7500‐year record of fire and precipitation dynamics from Clear Pond, South Carolina, USA

C. Anderson, Chad S. Lane, Zachary P. Taylor, Elizabeth A. Yanuskiewicz et al.
Journal of Quaternary Science
Geology and Paleoclimatology Research
article

A 7500‐year record of fire and precipitation dynamics from Clear Pond, South Carolina, USA

C. Anderson, Chad S. Lane, Zachary P. Taylor, Elizabeth A. Yanuskiewicz, Grace X. Pleasant
article en

Abstract

ABSTRACT We analyzed a 2.38 m sediment core from Clear Pond, South Carolina, to reconstruct fire and effective moisture over the past 7500 years in a Pinus ‐ Quercus forest. Our record of macroscopic charcoal, reconstructed precipitation isotopes from δ 2 H n‐alkane analysis, and other geochemical indicators provides a high‐resolution record of the interplays between fire and effective moisture on the Atlantic Coastal Plain (ACP). Our work complements and updates an existing pollen and microscopic charcoal record from Clear Pond with additional analyses, including reconstructed effective moisture. δ 2 H n‐alkane values are indicative of soil moisture isotopic values, which are controlled by precipitation δ 2 H values and fractionation during evaporation and transpiration. Our results show that from ca. 7500–3670 cal yr bp , effective moisture was higher than modern conditions at Clear Pond, but fires were frequent. Our δ 2 H n‐alkane record of effective moisture indicates that conditions remained mesic from ca. 3670 cal yr bp until 2350 cal yr bp , but macroscopic charcoal data indicate that fires were much less frequent than before. This pattern is in opposition to several nearby records on the ACP, where much of this timespan was apparently somewhat dry with frequent fires. After ca. 2350 cal yr bp , effective moisture slightly increased, and frequent fires returned to the landscape. These conditions persisted until about ca. 860 cal yr bp , when δ 2 H‐derived effective moisture values reached their most positive values, indicating xeric conditions, and charcoal data indicate a declining importance of fire on the landscape. Over the past 7500 years at Clear Pond, there is an apparent decoupling of reconstructed paleomoisture indicators and macroscopic charcoal records, which indicates that fire is not largely controlled by climate on the ACP and that landscape burning by Native Americans may be an important control on Holocene fire regimes at Clear Pond, especially from ca. 7500–2350 cal yr bp .

Journal of Quaternary ScienceVol. 40(5)
Berry College (US), University of Miami (US), University of North Carolina Wilmington (US)
Berry College
Openalex Percentile: Top 88%
Geology and Paleoclimatology Research
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