Abstract

The present study performed in Horten Inner Harbor (southern Norway) shows that foraminifera link the present-day Ecological Quality Status (EcoQS) to EcoQS of former times and, this way, bridge an important knowledge gap concerning determination of reference conditions, even in naturally stressed environments such as transitional waters and oxygen depleted habitats. In Horten Inner Harbor, geochemical data in the oldest deposits showed stable background concentrations for about 200 years (from about 1600 to 1800) before human activity became noteworthy, reflecting ‘good’ to ‘high’ status. Hence, it is reasonable that organisms, which lived in the area during the same nearly un-impacted time interval, represent the biologically defined reference conditions, irrespectively of whether the biotic indices are classified as ‘good’ or ‘bad’. The present paper illustrates, with a conceptual model, how the retrospective foraminiferal biomonitoring method can be used to detect environmental perturbations in estuaries and meet the difficulties of the Estuarine Quality Paradox.

Highlights

  • Fjords are a type of estuary (e.g., Syvitski et al, 1987)

  • The present study performed in Horten Inner Harbor shows that foraminifera link the presentday Ecological Quality Status (EcoQS) to EcoQS of former times and, this way, bridge an important knowledge gap concerning determination of reference conditions, even in naturally stressed environments such as transi­ tional waters and oxygen depleted habitats

  • It is reasonable that organisms, which lived in the area during the same nearly un-impacted time interval, represent the biologically defined reference conditions, irrespectively of whether the biotic indices are classified as ‘good’ or ‘bad’

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Summary

Introduction

Fjords are a type of estuary (e.g., Syvitski et al, 1987) They are relatively sheltered coastal marine areas, often with a naturally stressed environment due to the presence of one or more sills, estuarine circu­ lation with high fresh-water input, stratified water columns, and irreg­ ular deep-water exchange that may lead to natural oxygen depletion. They are commonly preferential urbanization areas and exposed to domestic and industrial effluents.

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