Arid
DOI10.1177/0959683619895580
Holocene climate variability of the Western Mediterranean: Surface water dynamics inferred from calcareous plankton assemblages
Bazzicalupo, Pietro1; Maiorano, Patrizia1; Girone, Angela1; Marino, Maria1; Combourieu-Nebout, Nathalie2; Pelosi, Nicola3; Salgueiro, Emilia4,5; Incarbona, Alessandro6
通讯作者Bazzicalupo, Pietro
来源期刊HOLOCENE
ISSN0959-6836
EISSN1477-0911
出版年2020
卷号30期号:5页码:691-708
英文摘要A high-resolution study (centennial scale) has been performed on the calcareous plankton assemblage of the Holocene portion of the Ocean Drilling Program Site 976 (Alboran Sea) with the aim to identify the main changes in the surface water dynamic. The dataset also provided a seasonal foraminiferal sea surface water temperatures (SSTs), estimated using the modern analog technique SIMMAX 28, and it was compared with available geochemical and pollen data at the site. Three main climate shifts were identified as (1) the increase in abundance of Syracosphaera spp. and Turborotalita quinqueloba marks the early Holocene humid phase, during maximum summer insolation and enhanced river runoff. It is concomitant with the expansion of Quercus, supporting high humidity on land. It ends at 8.2 ka, registering a sudden temperature and humidity reduction; (2) the rise in the abundances of Florisphaera profunda and Globorotalia inflata, at ca. 8 ka, indicates the development of the modern geostrophic front, gyre circulation, and of a deep nutricline following the sea-level rise; and (3) the increase of small Gephyrocapsa and Globigerina bulloides at 5.3 ka suggests enhanced nutrient availability in surface waters, related to more persistent wind-induced upwelling conditions. Relatively higher winter SST in the last 3.5 ka favored the increase of Trilobatus sacculifer, likely connected to more stable surface water conditions. Over the main trends, a short-term cyclicity is registered in coccolithophore productivity during the last 8 ka. Short periods of increased productivity are in phase with Atlantic waters inflow, and more arid intervals on land. This cyclicity has been related with periods of positive North Atlantic Oscillation (NAO) circulations. Spectral analysis on coccolithophore productivity confirms the occurrence of millennial-scale cyclicity, suggesting an external (i.e. solar) and an internal (i.e. atmospheric/oceanic) forcing.
英文关键词Alboran Sea coccolithophores foraminifera Holocene millennial-centennial-scale climate variability paleoclimate paleoproductivity
类型Article
语种英语
国家Italy ; France ; Portugal
开放获取类型Green Submitted
收录类别SCI-E
WOS记录号WOS:000507185400001
WOS关键词NORTH-ATLANTIC OSCILLATION ; LAST GLACIAL MAXIMUM ; ALBORAN-SEA ; MILLENNIAL-SCALE ; DEEP-WATER ; LATE QUATERNARY ; OCEANOGRAPHIC CHANGES ; DANSGAARD-OESCHGER ; MIDDLE PLEISTOCENE ; SAPROPEL FORMATION
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
EI主题词2020-01-03
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/312379
作者单位1.Univ Bari Aldo Moro, Dipartimento Sci Terra & Geoambientali, Via Edoardo Orabona 4, I-70125 Bari, Italy;
2.French Natl Ctr Sci Res, UMR 7194 Hist Nat Homme Prehist, Paris, France;
3.CNR, Ist Sci Marine ISMAR, Calata Porta Di Massa, Italy;
4.IPMA, Div Geol & Georecursos Marinhos, Lisbon, Portugal;
5.Univ Algarve, Ctr Marine Sci, Faro, Portugal;
6.Univ Palermo, Dipartimento Sci Terra & Mare, Palermo, Italy
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GB/T 7714
Bazzicalupo, Pietro,Maiorano, Patrizia,Girone, Angela,et al. Holocene climate variability of the Western Mediterranean: Surface water dynamics inferred from calcareous plankton assemblages[J],2020,30(5):691-708.
APA Bazzicalupo, Pietro.,Maiorano, Patrizia.,Girone, Angela.,Marino, Maria.,Combourieu-Nebout, Nathalie.,...&Incarbona, Alessandro.(2020).Holocene climate variability of the Western Mediterranean: Surface water dynamics inferred from calcareous plankton assemblages.HOLOCENE,30(5),691-708.
MLA Bazzicalupo, Pietro,et al."Holocene climate variability of the Western Mediterranean: Surface water dynamics inferred from calcareous plankton assemblages".HOLOCENE 30.5(2020):691-708.
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