Orbital control on the timing of oceanic anoxia in the Late Cretaceous

Autor: S. J. Batenburg, D. De Vleeschouwer, M. Sprovieri, F. J. Hilgen, A. S. Gale, B. S. Singer, C. Koeberl, R. Coccioni, P. Claeys, A. Montanari

Publikováno v: Climate of the Past, Vol 12, Iss 10, Pp 1995-2009 (2016)

The oceans at the time of the Cenomanian–Turonian transition were abruptly perturbed by a period of bottom-water anoxia. This led to the brief but widespread deposition of black organic-rich shales, such as the Livello Bonarelli in the Umbria–Mar

Externí odkaz: https://doaj.org/article/54e42fe86b2a48f4b966a14ae70db6b6

The calcareous nannofossil Prinsiosphaera achieved rock-forming abundances in the latest Triassic of western Tethys: consequences for the δ13C of bulk carbonate

Autor: N. Preto, C. Agnini, M. Rigo, M. Sprovieri, H. Westphal

Publikováno v: Biogeosciences, Vol 10, Iss 9, Pp 6053-6068 (2013)

The onset of pelagic biomineralization was a milestone in the history of the long-term inorganic carbon cycle: as soon as calcareous nannofossils became major limestone producers, the pH and supersaturation state of the global ocean were stabilized (

Externí odkaz: https://doaj.org/article/ee636d58471b4adb9c8fd3ab41f64beb

The Impact of the Little Ice Age on Coccolithophores in the Central Mediterranea Sea

Autor: A. Incarbona, P. Ziveri, E. Di Stefano, F. Lirer, G. Mortyn, B. Patti, N. Pelosi, M. Sprovieri, G. Tranchida, M. Vallefuoco, S. Albertazzi, L. G. Bellucci, A. Bonanno, S. Bonomo, P. Censi, L. Ferraro, S. Giuliani, S. Mazzola, R. Sprovieri

Publikováno v: Climate of the Past, Vol 6, Iss 6, Pp 795-805 (2010)

The Little Ice Age (LIA) is the last episode of a series of Holocene climatic anomalies. There is still little knowledge on the response of the marine environment to the pronounced cooling of the LIA and to the transition towards the 20th century glo

Externí odkaz: https://doaj.org/article/9c245c6a519e45d9989b8a213332807a

Assessing the impact of the Asian mussel Arcuatula senhousia in the recently invaded Oristano Lagoon-Gulf system (W Sardinia, Italy)

Autor: Sara Saba, Serena Como, P. Rumolo, Antonello Floris, Antonio Pais, M. Sprovieri, Paolo Magni

Publikováno v: Estuarine, coastal and shelf science (Online) (2015). doi:10.1016/j.ecss.2015.11.024
info:cnr-pdr/source/autori:Como, S; Floris, A; Pais, A; Rumolo, P; Saba, S; Sprovieri, M; Magni, P/titolo:Assessing the impact of the Asian mussel Arcuatula senhousia in the recently invaded Oristano Lagoon-Gulf system (W Sardinia, Italy)./doi:10.1016%2Fj.ecss.2015.11.024/rivista:Estuarine, coastal and shelf science (Online)/anno:2015/pagina_da:/pagina_a:/intervallo_pagine:/volume

In the marine environment, the introduction and spread of non-indigenous mussels may cause major modifications to native assemblages and alter the trophic flow within the food web. We analysed the impacts of the recently sighted Asian date mussel Arc

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::60c30dca8fc5d7686e89246c8b5990bc
https://doi.org/10.1016/j.ecss.2015.11.024

THE CAPO ROSSELLO BORE-HOLE (AGRIGENTO, SICILY) CYCLOSTRATIGRAPHIC AND PALEOCEANOGRAPHIC RECONSTRUCTIONS FROM QUANTITATIVE ANALYSES OF THE ZANCLEAN FORAMINIFERAL ASSEMBLAGES

Autor: F. SGARRELLA, R. SPROVIERI, E. DI STEFANO, A. CARUSO, M. SPROVIERI, G. BONADUCE

Publikováno v: Rivista Italiana di Paleontologia e Stratigrafia, Vol 105, Iss 2 (1999)

Cyclostratigraphy based on the quantitative analyses of planktonic foraminifera in the Zanclean segment (M Pl 1 base of M Pl 3 biozones) of the bore-hole drilled in the Capo Rossello area (Sicily, Southern Italy) allows us to recognize that the calca

Externí odkaz: https://doaj.org/article/7d08c0500a9d42ccba489f15ab8ef2c4