1GRC Geociències Marines, Departament de Dinàmica de la
Terra i de l'Oceà, Facultat de Geologia, Universitat de Barcelona,
Barcelona, Spain
2Institut de Ciència i Tecnologia Ambientals & Departament de
Física, Universitat Autònoma de Barcelona, Bellaterra, Spain
3School of Natural Sciences and Centre for Marine Ecosystems
Research, Edith Cowan University, Joondalup, Australia
4Oceans Institute and School of Physics, The University of Western
Australia, Crawley, Australia
5Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA),
Consell Superior d'Investigacions Científiques (CSIC), Barcelona, Spain
6Istituto per l'Ambiente Marino Costiero (IAMC)–Consiglio Nazionale
delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133,
Naples, Italy
1GRC Geociències Marines, Departament de Dinàmica de la
Terra i de l'Oceà, Facultat de Geologia, Universitat de Barcelona,
Barcelona, Spain
2Institut de Ciència i Tecnologia Ambientals & Departament de
Física, Universitat Autònoma de Barcelona, Bellaterra, Spain
3School of Natural Sciences and Centre for Marine Ecosystems
Research, Edith Cowan University, Joondalup, Australia
4Oceans Institute and School of Physics, The University of Western
Australia, Crawley, Australia
5Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA),
Consell Superior d'Investigacions Científiques (CSIC), Barcelona, Spain
6Istituto per l'Ambiente Marino Costiero (IAMC)–Consiglio Nazionale
delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133,
Naples, Italy
Received: 28 Sep 2015 – Discussion started: 18 Nov 2015 – Revised: 10 Mar 2016 – Accepted: 13 Mar 2016 – Published: 07 Apr 2016
Abstract. This study presents the reconstructed evolution of sea surface conditions in the central-western Mediterranean Sea during the late Holocene (2700 years) from a set of multi-proxy records as measured on five short sediment cores from two sites north of Minorca (cores MINMC06 and HER-MC-MR3). Sea surface temperatures (SSTs) from alkenones and Globigerina bulloides Mg / Ca ratios are combined with δ18O measurements in order to reconstruct changes in the regional evaporation–precipitation (E–P) balance. We also revisit the G. bulloides Mg / Ca–SST calibration and re-adjusted it based on a set of core-top measurements from the western Mediterranean Sea. Modern regional oceanographic data indicate that Globigerina bulloides Mg / Ca is mainly controlled by seasonal spring SST conditions, related to the April–May primary productivity bloom in the region. In contrast, the alkenone–SST signal represents an integration of the annual signal.
The construction of a robust chronological framework in the region allows for the synchronization of the different core sites and the construction of “stacked” proxy records in order to identify the most significant climatic variability patterns. The warmest sustained period occurred during the Roman Period (RP), which was immediately followed by a general cooling trend interrupted by several centennial-scale oscillations. We propose that this general cooling trend could be controlled by changes in the annual mean insolation. Even though some particularly warm SST intervals took place during the Medieval Climate Anomaly (MCA), the Little Ice Age (LIA) was markedly unstable, with some very cold SST events mostly during its second half. Finally, proxy records for the last centuries suggest that relatively low E–P ratios and cold SSTs dominated during negative North Atlantic Oscillation (NAO) phases, although SSTs seem to present a positive connection with the Atlantic Multidecadal Oscillation (AMO) index.
We present a high-resolution multi-proxy study about the evolution of sea surface conditions along the last 2700 yr in the north-western Mediterranean Sea based on five sediment records from two different sites north of Minorca. The novelty of the results and the followed approach, constructing stack records from the studied proxies to preserve the most robust patterns, provides a special value to the study. This complex period appears to have significant regional changes in the climatic signal.
We present a high-resolution multi-proxy study about the evolution of sea surface conditions...
