Premium
Establishing temperate crustose early Holocene coralline algae as archives for palaeoenvironmental reconstructions of the shallow water habitats of the Mediterranean Sea
Author(s) -
Ragazzola Federica,
Caragnano Annalisa,
Basso Daniela,
Schmidt Daniela N.,
Fietzke Jan
Publication year - 2020
Publication title -
palaeontology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.69
H-Index - 63
eISSN - 1475-4983
pISSN - 0031-0239
DOI - 10.1111/pala.12447
Subject(s) - coralline algae , crustose , temperate climate , oceanography , paleontology , ecology , algae , geology , holocene , biology
Abstract Over the past decades, coralline algae have increasingly been used as archives of palaeoclimate information due to their seasonal growth bands and their vast distribution from high latitudes to the tropics. Traditionally, these reconstructions have been performed mainly on high latitude species, limiting the geographical area of their potential use. Here we assess the use of temperate crustose fossil coralline algae from shallow water habitats for palaeoenvironmental reconstruction to generate records of past climate change. We determine the potential of three different species of coralline algae, Lithothamnion minervae , Lithophyllum stictaeforme and Mesophyllum philippii , with different growth patterns, as archives for pH (δ 11 B) and temperature (Mg/Ca) reconstruction in the Mediterranean Sea. Mg concentration is driven by temperature but modulated by growth rate, which is controlled by species‐specific and intraspecific growth patterns. L. minervae is a good temperature recorder, showing a moderate warming trend in specimens from 11.37 cal ka BP (from 14.2 ± 0.4°C to 14.9 ± 0.15°C) to today. In contrast to Mg, all genera showed consistent values of boron isotopes (δ 11 B) suggesting a common control on boron incorporation. The recorded δ 11 B in modern and fossil coralline specimens is in agreement with literature data about early Holocene pH , opening new perspectives of coralline‐based, high‐resolution pH reconstructions in deep time.