Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2020.110090 |
Nearshore paleoceanogaphic conditions through the Holocene: Shell carbonate from archaeological sites of the Atacama Desert coast | |
Flores, Carola; Broitman, Bernardo R. | |
通讯作者 | Flores, C (corresponding author), Univ Catolica Norte, Fac Ciencias Mar, Ctr Estudios Avanzados Zonas Aridas CEAZA, Ossandon 877, Coquimbo, Chile. |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2021 |
卷号 | 562 |
英文摘要 | From the southern coast of Peru to the central-north coast of Chile (18 degrees-31 degrees S) previous evidence suggests that wide variations in sea surface temperature (SST) over the Holocene may be associated with changes in coastal upwelling regimes along the region. Support for spatial contrasts and similarities in oceanographic dynamics comes from earlier work at both extremes of the region. Using a 12 kyr record derived from shell midden archaeological sites around Taltal Chile (25 degrees S), we show that changes in the region are not necessarily consistent with a simple latitudinal gradient. Using delta C-13 and delta O-18 isotopic records from archaeological carbonate shells of the keyhole limpet Fissurella maxima we find that cold SST during the Early Holocene was associated with more negative delta C-13 values in agreement with observations from southern Peru. Warmer waters during the beginning of the Middle Holocene, had positive delta C-13 values, differentiating them from southern Peru and central-north Chile records. The rest of the Middle Holocene showed a decreasing SST accompanied by negative delta C-13 values, and after 4000 cal yr BP, the Late Holocene showed a progressive increase in SST and positive delta C-13 values. Finally, modern carbonate shells of F. maxima indicate a situation not observed throughout the Holocene period: warm SST is associated with negative delta C-13 values, in line with results on modern shells from southern Peru and modern oceanographic patterns that indicate an intensification of coastal upwelling with events of warm water intrusion. Our results show that the southern coast of the Atacama Desert experienced important fluctuations in SST and upwelling conditions during the Holocene, which may have affected the distribution of nearshore fisheries along the Northern Coast of Chile. |
英文关键词 | Fissurella maxima shell Isotopic analysis delta O-18 delta C-13 Coastal upwelling Shell carbonate Sea surface temperature |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000604584600025 |
WOS关键词 | HUMBOLDT CURRENT SYSTEM ; SEA-SURFACE TEMPERATURE ; SANTA-CRUZ ISLAND ; MIDDLE HOLOCENE ; SOUTHEASTERN PACIFIC ; HYPERARID COAST ; OCEANIC UPTAKE ; RESERVOIR AGE ; CHILE ; PRODUCTIVITY |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/348082 |
作者单位 | [Flores, Carola] Univ Catolica Norte, Fac Ciencias Mar, Ctr Estudios Avanzados Zonas Aridas CEAZA, Ossandon 877, Coquimbo, Chile; [Broitman, Bernardo R.] Univ Adolfo Ibanez, Fac Artes Liberales, Dept Ciencias, Vina Del Mar, Chile; [Broitman, Bernardo R.] Univ Adolfo Ibanez, Bioengn Innovat Ctr, Fac Ingn & Ciencias, Vina Del Mar, Chile |
推荐引用方式 GB/T 7714 | Flores, Carola,Broitman, Bernardo R.. Nearshore paleoceanogaphic conditions through the Holocene: Shell carbonate from archaeological sites of the Atacama Desert coast[J],2021,562. |
APA | Flores, Carola,&Broitman, Bernardo R..(2021).Nearshore paleoceanogaphic conditions through the Holocene: Shell carbonate from archaeological sites of the Atacama Desert coast.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,562. |
MLA | Flores, Carola,et al."Nearshore paleoceanogaphic conditions through the Holocene: Shell carbonate from archaeological sites of the Atacama Desert coast".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 562(2021). |
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