Title
Late Neogene evolution of the Peruvian margin and its ecosystems: a synthesis from the Sacaco record
Date Issued
01 April 2021
Access level
open access
Resource Type
journal article
Publisher(s)
Springer Science and Business Media Deutschland GmbH
Abstract
The highly productive waters of the Humboldt Current System (HCS) host a particular temperate ecosystem within the tropics, whose history is still largely unknown. The Pisco Formation, deposited during Mio-Pliocene times in the Peruvian continental margin has yielded an outstanding collection of coastal-marine fossils, providing an opportunity to understand the genesis of the HCS ecosystem. We present a comprehensive review, completed with new results, that integrates geological and paleontological data from the last 10 My, especially focusing on the southern East Pisco Basin (Sacaco area). We discuss the depositional settings of the Pisco Formation and integrate new U/Pb radiometric ages into the chronostratigraphic framework of the Sacaco sub-basin. The last preserved Pisco sediments at Sacaco were deposited ~ 4.5 Ma, while the overlying Caracoles Formation accumulated from ~ 2.7 Ma onwards. We identified a Pliocene angular unconformity encompassing 1.7 My between these formations, associated with a regional phase of uplift. Local and regional paleoenvironmental indicators suggest that shallow settings influenced by the offshore upwelling of ventilated and warm waters prevailed until the early Pliocene. We present an extensive synthesis of the late Miocene–Pleistocene vertebrate fossil record, which allows for an ecological characterization of the coastal-marine communities, an assessment of biodiversity trends, and changes in coastal-marine lineages in relation to modern HCS faunas. Our synthesis shows that: (i) typical endemic coastal Pisco vertebrates persisted up to ~ 4.5 Ma, (ii) first modern HCS toothed cetaceans appear at ~ 7–6 Ma, coinciding with a decline in genus diversity, and (iii) a vertebrate community closer to the current HCS was only reached after 2.7 Ma. The genesis of the Peruvian coastal ecosystem seems to be driven by a combination of stepwise transformations of the coastal geomorphology related to local tectonic pulses and by a global cooling trend leading to the modern oceanic circulation system.
Start page
995
End page
1025
Volume
110
Issue
3
Language
English
OCDE Knowledge area
Ecología Ciencias del medio ambiente
Scopus EID
2-s2.0-85102393992
Source
International Journal of Earth Sciences
ISSN of the container
14373254
Sponsor(s)
This research was supported by the Peruvian Fondo Nacional de Desarrollo Científico, Tecnológico y de Innovación Tecnológica (FONDECYT) through the Programa de incorporación de investigadores (Grant Nº E038-2019-02-FONDECYT-Banco Mundial) and the MAGNET program (Contract Nº 07-2017-FONDECYT). Funding was also available through the Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica (CONCYTEC) –FONDECYT research grants 105-2018 and 104-2018 awarded to DO and RS-G, respectively. We especially thank R. Varas (UPCH, Peru), L. Pairazamán (UNI, Peru) and R. Berrospi (UNI, Peru) for logistical assistance during the second field campaign. PERUPETRO S.A. and Ysabel Calderón are thanked for providing access to seismic data. This manuscript greatly benefited from comments by J. Macharé, A. Collareta, R. Esperante, and C. DiCelma.
Sources of information: Directorio de Producción Científica Scopus