Zachary P. Taylor, Chelsea N. Anderson, Chad S. Lane, Grace X. Pleasant, Elizabeth Yanuskiewicz
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Our work complements and updates an existing pollen and microscopic charcoal record from Clear Pond with additional analyses, including reconstructed effective moisture. δ<sup>2</sup>H<sub><i>n-alkane</i></sub> values are indicative of soil moisture isotopic values, which are controlled by precipitation δ<sup>2</sup>H values and fractionation during evaporation and transpiration. Our results show that from ca. 7500–3670 cal yr \n<span>bp</span>, effective moisture was higher than modern conditions at Clear Pond, but fires were frequent. Our δ<sup>2</sup>H<sub><i>n-alkane</i></sub> record of effective moisture indicates that conditions remained mesic from ca. 3670 cal yr \n<span>bp</span> until 2350 cal yr \n<span>bp</span>, 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 \n<span>bp</span>, effective moisture slightly increased, and frequent fires returned to the landscape. These conditions persisted until about ca. 860 cal yr \n<span>bp</span>, when δ<sup>2</sup>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 \n<span>bp</span>.</p>\n </div>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"40 5","pages":"764-777"},"PeriodicalIF":2.2000,"publicationDate":"2025-04-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A 7500-year record of fire and precipitation dynamics from Clear Pond, South Carolina, USA\",\"authors\":\"Zachary P. Taylor, Chelsea N. Anderson, Chad S. Lane, Grace X. 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Our results show that from ca. 7500–3670 cal yr \\n<span>bp</span>, effective moisture was higher than modern conditions at Clear Pond, but fires were frequent. Our δ<sup>2</sup>H<sub><i>n-alkane</i></sub> record of effective moisture indicates that conditions remained mesic from ca. 3670 cal yr \\n<span>bp</span> until 2350 cal yr \\n<span>bp</span>, 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 \\n<span>bp</span>, effective moisture slightly increased, and frequent fires returned to the landscape. These conditions persisted until about ca. 860 cal yr \\n<span>bp</span>, when δ<sup>2</sup>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. 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引用次数: 0
摘要
我们分析了来自南卡罗来纳州Clear Pond的2.38 m沉积物岩心,以重建过去7500年松树-栎林的火灾和有效湿度。我们的宏观碳记录、δ 2hn -烷烃分析重建的降水同位素和其他地球化学指标提供了大西洋沿岸平原(ACP)火与有效水分相互作用的高分辨率记录。我们的工作补充和更新了Clear Pond现有的花粉和微观木炭记录,并进行了额外的分析,包括重建的有效水分。δ2H烷烃值指示土壤水分同位素值,而土壤水分同位素值受降水δ2H值和蒸发蒸腾分馏的控制。结果表明,在约7500 ~ 3670 cal yr bp期间,清塘的有效湿度高于现代条件,但火灾频繁发生。我们的δ 2n -烷烃有效水分记录表明,从约3670 cal - yr bp到2350 cal - yr bp,条件保持稳定,但宏观木炭数据表明,火灾比以前少得多。这一模式与ACP附近的几个记录相反,其中大部分时间显然有些干燥,经常发生火灾。在大约2350 calyr bp之后,有效水分略有增加,并且频繁的火灾再次出现在景观中。这些条件一直持续到大约860 cal yr bp,此时δ 2h导出的有效水分值达到最大值,表明干旱条件,木炭数据表明火对景观的重要性正在下降。在过去的7500年里,重建的古湿度指标与宏观木炭记录之间存在明显的解耦合,这表明ACP上的火灾在很大程度上不受气候的控制,美洲原住民的景观燃烧可能是clearpond全新世火灾的重要控制因素,特别是在约7500 - 2350 cal yr bp之间。
A 7500-year record of fire and precipitation dynamics from Clear Pond, South Carolina, USA
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 δ2Hn-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. δ2Hn-alkane values are indicative of soil moisture isotopic values, which are controlled by precipitation δ2H 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 δ2Hn-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 δ2H-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.
期刊介绍:
The Journal of Quaternary Science publishes original papers on any field of Quaternary research, and aims to promote a wider appreciation and deeper understanding of the earth''s history during the last 2.58 million years. Papers from a wide range of disciplines appear in JQS including, for example, Archaeology, Botany, Climatology, Geochemistry, Geochronology, Geology, Geomorphology, Geophysics, Glaciology, Limnology, Oceanography, Palaeoceanography, Palaeoclimatology, Palaeoecology, Palaeontology, Soil Science and Zoology. The journal particularly welcomes papers reporting the results of interdisciplinary or multidisciplinary research which are of wide international interest to Quaternary scientists. Short communications and correspondence relating to views and information contained in JQS may also be considered for publication.