Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy)
We present the results of a high resolution study carried out on a shallow water sediment core, recovered in the central Tyrrhenian Sea to reconstruct the runoff story of the catchment basin of Volturno and Garigliano rivers (Gulf of Gaeta, Italy), over the past ~400years. We compared the abundance...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
---|---|
Main Authors: | , , , , , , , , , , |
Other Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2016
|
Subjects: | |
Online Access: | http://hdl.handle.net/2122/11507 https://doi.org/10.1016/j.palaeo.2016.06.037 |
id |
ftingv:oai:www.earth-prints.org:2122/11507 |
---|---|
record_format |
openpolar |
spelling |
ftingv:oai:www.earth-prints.org:2122/11507 2023-05-15T17:31:41+02:00 Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) Bonomo, S. Cascella, Antonio Alberico, I. Sorgato, S. Pelosi, N. Ferraro, L. Lirer, F. Vallefuoco, M. Bellucci, L. Agnini, C. Pappone, G. 1Istituto per l’Ambiente Marino Costiero, Consiglio Nazionale delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133 Napoli, Italy; 2Istituto di Biomedicina ed Immunologia Molecolare “Alberto Monroy” (IBIM), Consiglio Nazionale delle Ricerche, Via Ugo La Malfa 153, 90146, Palermo, Italy. Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia Istituto per l’Ambiente Marino Costiero (IAMC), Consiglio Nazionale delle Ricerche, Calata Porta di Massa, 80133, Napoli, Italy; Università degli Studi di Padova, Dipartimento di Geoscienze, Padova, Italy Istituto per l'Ambiente Marino Costiero (IAMC), Consiglio Nazionale delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133 Napoli, Italy Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche, Via Gobetti 101, 40129 Bologna, Italy Università degli Studi “Parthenope” di Napoli, Dipartimento di Scienze per l’Ambiente, Naples, Italy 2016 http://hdl.handle.net/2122/11507 https://doi.org/10.1016/j.palaeo.2016.06.037 en eng Palaeogeography, Palaeoclimatology, Palaeoecology /459 (2016) http://hdl.handle.net/2122/11507 doi:10.1016/j.palaeo.2016.06.037 open reworked coccoliths as runoff proxy article 2016 ftingv https://doi.org/10.1016/j.palaeo.2016.06.037 2022-07-29T06:07:26Z We present the results of a high resolution study carried out on a shallow water sediment core, recovered in the central Tyrrhenian Sea to reconstruct the runoff story of the catchment basin of Volturno and Garigliano rivers (Gulf of Gaeta, Italy), over the past ~400years. We compared the abundance distribution pattern of Reworked Coccoliths to the surface runoff model simulation for the Volturno and Garigliano rivers hydrographic basins, the Global Historical Climatology Network index, the Palmer drought severity index, the Tevere river discharge anomaly, the summer average rainfall of the Southern Italy and the North Atlantic Oscillation reconstructed signal. This comparison suggested that the biotic signal of the Reworked Coccoliths may be used to detect climatic events from local to “global” scale. The calcareous nannofossil assemblages as well as their diversity index are modulated by oscillation in solar activity, where minima in solar activity correspond to minima calcareous nannofossil diversity and viceversa. In particular, the antiphase correlation between the abundance of Reworked Coccoliths and the North Atlantic Oscillation index, which modulates the winter precipitation, suggests that this biotic index could be used as a reliable proxy to reconstruct the variations in the hydrographic basin runoff of the Volturno and Garigliano rivers. In addition, power spectral and wavelet analysis carried out on both signals documented the occurrence of climatic cycles of the duration of about 95yr. From 1900 AD upwards, a turnover in the periodicity from 95yr climatic cycles to 22-26 yr cycles occurred in the Reworked Coccoliths signal, suggesting a strong control of solar forcing (Hale cycle) over the last century. Published 15-28 5A. Paleoclima e ricerche polari JCR Journal Article in Journal/Newspaper North Atlantic North Atlantic oscillation Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Hale ENVELOPE(-86.317,-86.317,-78.067,-78.067) Palaeogeography, Palaeoclimatology, Palaeoecology 459 15 28 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
reworked coccoliths as runoff proxy |
spellingShingle |
reworked coccoliths as runoff proxy Bonomo, S. Cascella, Antonio Alberico, I. Sorgato, S. Pelosi, N. Ferraro, L. Lirer, F. Vallefuoco, M. Bellucci, L. Agnini, C. Pappone, G. Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) |
topic_facet |
reworked coccoliths as runoff proxy |
description |
We present the results of a high resolution study carried out on a shallow water sediment core, recovered in the central Tyrrhenian Sea to reconstruct the runoff story of the catchment basin of Volturno and Garigliano rivers (Gulf of Gaeta, Italy), over the past ~400years. We compared the abundance distribution pattern of Reworked Coccoliths to the surface runoff model simulation for the Volturno and Garigliano rivers hydrographic basins, the Global Historical Climatology Network index, the Palmer drought severity index, the Tevere river discharge anomaly, the summer average rainfall of the Southern Italy and the North Atlantic Oscillation reconstructed signal. This comparison suggested that the biotic signal of the Reworked Coccoliths may be used to detect climatic events from local to “global” scale. The calcareous nannofossil assemblages as well as their diversity index are modulated by oscillation in solar activity, where minima in solar activity correspond to minima calcareous nannofossil diversity and viceversa. In particular, the antiphase correlation between the abundance of Reworked Coccoliths and the North Atlantic Oscillation index, which modulates the winter precipitation, suggests that this biotic index could be used as a reliable proxy to reconstruct the variations in the hydrographic basin runoff of the Volturno and Garigliano rivers. In addition, power spectral and wavelet analysis carried out on both signals documented the occurrence of climatic cycles of the duration of about 95yr. From 1900 AD upwards, a turnover in the periodicity from 95yr climatic cycles to 22-26 yr cycles occurred in the Reworked Coccoliths signal, suggesting a strong control of solar forcing (Hale cycle) over the last century. Published 15-28 5A. Paleoclima e ricerche polari JCR Journal |
author2 |
1Istituto per l’Ambiente Marino Costiero, Consiglio Nazionale delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133 Napoli, Italy; 2Istituto di Biomedicina ed Immunologia Molecolare “Alberto Monroy” (IBIM), Consiglio Nazionale delle Ricerche, Via Ugo La Malfa 153, 90146, Palermo, Italy. Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia Istituto per l’Ambiente Marino Costiero (IAMC), Consiglio Nazionale delle Ricerche, Calata Porta di Massa, 80133, Napoli, Italy; Università degli Studi di Padova, Dipartimento di Geoscienze, Padova, Italy Istituto per l'Ambiente Marino Costiero (IAMC), Consiglio Nazionale delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133 Napoli, Italy Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche, Via Gobetti 101, 40129 Bologna, Italy Università degli Studi “Parthenope” di Napoli, Dipartimento di Scienze per l’Ambiente, Naples, Italy |
format |
Article in Journal/Newspaper |
author |
Bonomo, S. Cascella, Antonio Alberico, I. Sorgato, S. Pelosi, N. Ferraro, L. Lirer, F. Vallefuoco, M. Bellucci, L. Agnini, C. Pappone, G. |
author_facet |
Bonomo, S. Cascella, Antonio Alberico, I. Sorgato, S. Pelosi, N. Ferraro, L. Lirer, F. Vallefuoco, M. Bellucci, L. Agnini, C. Pappone, G. |
author_sort |
Bonomo, S. |
title |
Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) |
title_short |
Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) |
title_full |
Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) |
title_fullStr |
Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) |
title_full_unstemmed |
Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy) |
title_sort |
reworked coccoliths as runoff proxy for the last 400 years: the case of gaeta gulf (central tyrrhenian sea, central italy) |
publishDate |
2016 |
url |
http://hdl.handle.net/2122/11507 https://doi.org/10.1016/j.palaeo.2016.06.037 |
long_lat |
ENVELOPE(-86.317,-86.317,-78.067,-78.067) |
geographic |
Hale |
geographic_facet |
Hale |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
Palaeogeography, Palaeoclimatology, Palaeoecology /459 (2016) http://hdl.handle.net/2122/11507 doi:10.1016/j.palaeo.2016.06.037 |
op_rights |
open |
op_doi |
https://doi.org/10.1016/j.palaeo.2016.06.037 |
container_title |
Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
459 |
container_start_page |
15 |
op_container_end_page |
28 |
_version_ |
1766129367717511168 |