0000000000429275

AUTHOR

Jonathan A. Holmes

showing 2 related works from this author

The stable isotope composition of organic and inorganic fossils in lake sediment records: current understanding, challenges, and future directions

2018

This paper provides an overview of stable isotope analysis (H, C, N, O, Si) of the macro- and microscopic remains from aquatic organisms found in lake sediment records and their application in (palaeo)environmental science. Aquatic organisms, including diatoms, macrophytes, invertebrates, and fish, can produce sufficiently robust remains that preserve well as fossils and can be identified in lake sediment records. Stable isotope analyses of these remains can then provide valuable insights into habitat-specific biogeochemistry, feeding ecology, but also on climatic and hydrological changes in and around lakes. Since these analyses focus on the remains of known and identified organisms, they …

010506 paleontologyArcheologyTaphonomy010504 meteorology & atmospheric sciencesorganic remainsstable isotopessedimentit580 Plants (Botany)01 natural sciencesInorganic remainsäyriäisetIsotope fractionationpiilevätEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesIsotope analysisStable isotopesDiatomsGlobal and Planetary Changeinorganic remainsisotoopitEcologyStable isotope ratioLake ecosystemBiogeochemistryOstracodsGeologyselkärangattomatInvertebratespaleolimnologiaMacrophytelake sedimentLake sedimentostracodsOrganic remainsPaleoecologyEnvironmental science
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The influence of climate and sea-level change on the Holocene evolution of a Mediterranean coastal lagoon: Evidence from ostracod palaeoecology and g…

2013

Abstract Coastal lagoons provide an excellent basis for the study of processes controlling the evolution of a coastal zone. We examine the relative importance of these processes during the middle to late Holocene through a study of an 8.5 meter-long sediment record from the Albufera de Valencia (Spain). We combine sedimentological analyses with investigations into the palaeoecology, taphonomy and geochemistry (Mg/Ca, Sr/Ca, δ 18 O and δ 13 C) of ostracod valves in order to assess the effects of sea-level changes, storm events and effective moisture on the evolution of a Western Mediterranean coastal wetland. The late Pleistocene sediments represent a subaerial environment, which was followe…

Mediterranean climatebiologyPleistoceneGeochemistryPaleontologybiology.organism_classificationDeposition (geology)OceanographySpace and Planetary ScienceOstracodPaleoecologyProgradationHoloceneGeologyMarine transgressionGeobios
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