Knowledge Resource Center for Ecological Environment in Arid Area
| DOI | 10.18172/cig.2696 |
| THE UPPER PLEISTOCENE DEGLACIATION ON THE APENNINES (PENINSULAR ITALY) | |
| Giraudi, C. | |
| 通讯作者 | Giraudi, C |
| 来源期刊 | CUADERNOS DE INVESTIGACION GEOGRAFICA
 |
| ISSN | 0211-6820 |
| EISSN | 1697-9540 |
| 出版年 | 2015 |
| 卷号 | 41期号:2页码:337-358 |
| 英文摘要 | The synthesis of the published data and new researches allow to establish a more reliable chronology of the phases of deglaciation that occurred after the Apennine last glacial maximum. The chronological framework was assured by radiocarbon dating and by the presence of four geochemically and chronologically characterized tephra layers and a quartz-rich loess, that were found on different mountain massifs, mainly in Central Italy. After the Campo Imperatore Stade (local LGM) dated 28-27 ka cal BP, a first retreat took place during the Campo Felice Arid Spell, followed by a glaciers advance (Le Capannelle Stade) that started between 26 and 25 ka cal BP. During the readvance the glaciers reached a length about 90% of the local LGM glacier. The readvance was followed by a retreat broken by at least two readvances (Piano Pietranzoni and Lago Pietranzoni readvances) and then by a very fast withdrawal at the beginning of the Fornaca Interstade, dated ca. 22-21 ka cal BP. The Fontari Stade glacier's advance began ca. 18 ka cal BP and was followed by a retreat broken by at least three small readvances (Fontari 2; Fontari 3; M. Aquila 1). The M. Aquila 1 readvance ended ca. 15-14 ka cal BP. The Venaquaro Interstade, dated 14-13 ka cal BP, was followed by the M. Aquila Stade. This stade was the last Late Pleistocene small glacial expansion and can be correlated to the Younger Dryas. The variations in the atmospheric circulation in the Mediterranean area likely played a role during the first deglaciation phases (between 27-26 and 21-22 ka cal BP). During the period between 19-18 and 12 ka cal BP the glacial fluctuations were linked, very likely, to the climatic impact of the North Atlantic ice rafted debris events. It is possible, therefore, that during the Fornaca Interstade (between 22-21 and 19-18 ka cal BP), there has been such a change in atmospheric circulation and the Central Mediterranean area became more prone to be influenced by the effects of the North Atlantic D/O and IRD events. |
| 英文关键词 | peninsular Italy Apennines late Upper Pleistocene deglaciation glacial phases tephra layers proglacial lacustrine sediments |
| 类型 | Article |
| 语种 | 英语 |
| 开放获取类型 | DOAJ Gold |
| 收录类别 | ESCI |
| WOS记录号 | WOS:000374194300006 |
| WOS关键词 | GRANDE-DI-MONTICCHIO ; VEGETATION HISTORY ; MEDITERRANEAN MOUNTAINS ; ENVIRONMENTAL-CHANGES ; POLLEN STRATIGRAPHY ; SEDIMENT RECORD ; HOLOCENE ; PALEOCLIMATE ; OSCILLATIONS ; GLACIATION |
| WOS类目 | Geography, Physical |
| WOS研究方向 | Physical Geography |
| 资源类型 | 期刊论文 |
| 条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/331236 |
| 作者单位 | [Giraudi, C.] ENEA, CR Saluggia, Str Crescentino 41, I-13040 Saluggia, Italy |
| 推荐引用方式 GB/T 7714 | Giraudi, C.. THE UPPER PLEISTOCENE DEGLACIATION ON THE APENNINES (PENINSULAR ITALY)[J],2015,41(2):337-358. |
| APA | Giraudi, C..(2015).THE UPPER PLEISTOCENE DEGLACIATION ON THE APENNINES (PENINSULAR ITALY).CUADERNOS DE INVESTIGACION GEOGRAFICA,41(2),337-358. |
| MLA | Giraudi, C.."THE UPPER PLEISTOCENE DEGLACIATION ON THE APENNINES (PENINSULAR ITALY)".CUADERNOS DE INVESTIGACION GEOGRAFICA 41.2(2015):337-358. |
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