Abstract

We developed an algorithm to improve richness assessment based on paleoecological series, considering sample features such as their temporal resolutions or their volumes. Our new method can be applied to both high- and low-count size proxies, i.e. pollen and plant macroremain records, respectively. While pollen generally abounds in sediments, plant macroremains are generally rare, thus leading to difficulties to compute paleo-biodiversity indices. Our approach uses resampled macroremain influxes that enable the computation of the rarefaction index for the low influx records. The raw counts are resampled to a constant resolution and sample volume by interpolating initial sample ages at a constant time interval using the age∼depth model. Then, the contribution of initial counts and volume to each interpolated sample is determined by calculating a proportion matrix that is in turn used to obtain regularly spaced time series of pollen and macroremain influx. We applied this algorithm to sedimentary data from a subalpine lake situated in the European Alps. The reconstructed total floristic richness at the study site increased gradually when both pollen and macroremain records indicated a decrease in relative abundances of shrubs and an increase in trees from 11,000 to 7,000 cal BP. This points to an ecosystem change that favored trees against shrubs, whereas herb abundance remained stable. Since 6,000 cal BP, local richness decreased based on plant macroremains, while pollen-based richness was stable. The reconstructed richness and evenness are interrelated confirming the difficulty to distinguish these two aspects for the studies in paleo-biodiversity. The present study shows that low-influx bio-proxy records (here macroremains) can be used to reconstruct stand diversity and address ecological issues. These developments on macroremain and pollen records may contribute to bridge the gap between paleoecology and biodiversity studies.

Highlights

  • Biodiversity-loss rates are actively investigated to determine their relationship with habitat fragmentation, climatic and social changes (e.g. [1]), there is a need to assess current rates against longer-term loss rates that occurred in response to past environmental change

  • We describe a new method to estimate and compare the taxonomic richness and evenness of vegetation based on pollen and plant-macrofossil records

  • Differences in taxonomic richness and evenness may occur between samples of the same sedimentary sequence because higher taxa numbers can be expected in samples of larger volumes, in samples that accumulated over a longer time span, and when count sizes are larger

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Summary

Introduction

Biodiversity-loss rates are actively investigated to determine their relationship with habitat fragmentation, climatic and social changes (e.g. [1]), there is a need to assess current rates against longer-term loss rates that occurred in response to past environmental change. [1]), there is a need to assess current rates against longer-term loss rates that occurred in response to past environmental change Such assessments could be valuable for highlighting the influence of ecological stress and disturbance on biodiversity [2]. Among several indices of species richness, the rarefaction method [3,4,5] is often used because it is effective for standardizing the species richness of assemblages of different sizes to a common number of individuals or samples, i.e., the ‘expected taxonomic richness, E(Tn)’ This standardization is necessary due to the non-linear relationship between richness and the number of individuals recorded. Examples include terrestrial plants (based on pollen e.g. [7,8,9]), algae (based on diatoms e.g. [10]), insects (from chironomids e.g. [11]) or testate amoebae [12]

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