The geochemistry of modern calcareous barnacle shells and applications for palaeoenvironmental studies

C.V Ullmann,A.S Gale,J Huggett,D Wray,R Frei,C Korte,S Broom-Fendley,K Littler,S.P Hesselbo

doi:10.1016/j.gca.2018.09.010

Abstract

Thoracican barnacles of the Superorder Thoracicalcarea Gale, 2016 are sessile calcifiers which are ubiquitous in the intertidal zone and present from very shallow to the deepest marine environments; they also live as epiplankton on animals and detritus. The geochemical composition of their shell calcite has been shown to yield information about environmental conditions, but comprehensive analyses of barnacle shell geochemistry are so far lacking.Here, a dataset is reported for Mg/Ca, Sr/Ca, Mn/Ca, Fe/Ca, as well as carbon and oxygen isotope ratios for 42 species from the Balaniformes, Verruciformes, Scalpelliformes and Lepadiformes. Barnacles predominantly form low-Mg-calcite with very high Sr/Ca ratios averaging 4.2 mmol/mol. The Mn/Ca and Fe/Ca ratios in shell plates are variable and can exceed >4 mmol/mol in barnacles that are attached to manmade structures or live close to (anthropogenic) sources of Mn and Fe. No strong phylogenetic control on the average element/Ca ratios is observed in barnacles. The Balaniformes show a ca. 40% enrichment of Mg in their scuta and terga as compared to other shell plates—a pattern which is not seen in other barnacles. The combination of low to medium Mg/Ca ratios and high Sr/Ca ratios is rare for marine biogenic calcite. Barnacles may thus become important for robustly reconstructing past seawater composition, if this signature is also present in fossil barnacle calcite and can be used alongside other fossil taxa with different Sr incorporation behaviour.Carbon and oxygen isotope data support the view that the oxygen isotope thermometer for barnacles is robust and that most barnacle species form their calcite near isotopic equilibrium with ambient water. The Lepadiformes, however, show a tendency for strong co-variation of δ13C with δ18O values and depletion in 13C and 18O which is attributed to isotopic disequilibrium during shell secretion.Strong systematic fluctuations in Mg/Ca ratios over length scales of ca. 5–15 µm are exhibited by the scalpelliform species Capitulum mitella, the only studied species which consistently forms high Mg calcite, and are tentatively linked to tidal control on the shell secretion pattern. Cathodoluminescence images for this species suggest that additionally a seasonal pattern of Mn distribution in its shell plates is recorded, pointing to a potential use for reconstruction of seasonal changes in terrestrial element supply.

Highlights

Barnacles have been of long-standing scientific interest with detailed work on taxonomy and fossil forms reaching back to Charles Darwin (e.g., Darwin, 1851, 1854)
Thoracican barnacles of the Superorder Thoracicalcarea Gale, 2016 are sessile calcifiers which are ubiquitous in the intertidal zone and present from very shallow to the deepest marine environments; they live as epiplankton on animals and detritus
Barnacles may become important for robustly reconstructing past seawater composition, if this signature is present in fossil barnacle calcite and can be used alongside other fossil taxa with different Sr incorporation behaviour

Summary

Introduction

Barnacles have been of long-standing scientific interest with detailed work on taxonomy and fossil forms reaching back to Charles Darwin (e.g., Darwin, 1851, 1854). Thoracican barnacles (subclass Cirripedia) first appeared in the Early Paleozoic (Briggs et al, 2005; Perez-Losada et al, 2008) and developed shells of phosphatic composition (Gale and Schweigert, 2016). Calcareous cirripedes first adapted to shallow marine hard substrates in the Late Cretaceous (Gale and Sørensen, 2015) and neobalanomorphs appeared in the Paleogene. These radiated rapidly, and by the Miocene these sessile forms were globally abundant and locally rock-forming in shallow marine habitats. Today they occupy a wide range of habitats from the intertidal zone down to deep sea trenches in the modern oceans (Foster, 1987)

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