0000000000515411

AUTHOR

Martin Kölling

0000-0003-2720-2211

showing 4 related works from this author

Last Interglacial Hydroclimate Seasonality Reconstructed From Tropical Atlantic Corals

2018

The seasonality of hydroclimate during past periods of warmer than modern global temperatures is a critical component for understanding future climate change scenarios. Although only partially analogous to these scenarios, the last interglacial (LIG, Marine Isotope Stage 5e, ~127–117 ka) is a popular test bed. We present coral δ18O monthly resolved records from multiple Bonaire (southern Caribbean) fossil corals (Diploria strigosa) that date to between 130 and 118 ka. These records represent up to 37 years and cover a total of 105 years, offering insights into the seasonality and characteristics of LIG tropical Atlantic hydroclimate. Our coral δ18O records and available coral Sr/Ca-sea surf…

Marine isotope stageAtmospheric ScienceDiploria strigosa010504 meteorology & atmospheric sciencesbiologyIntertropical Convergence ZoneCoralPaleontologyTropical AtlanticSeasonality010502 geochemistry & geophysicsOceanographymedicine.diseasebiology.organism_classificationAnnual cycle01 natural sciencesGeographyOceanography13. Climate actionInterglacialmedicine14. Life underwater0105 earth and related environmental sciencesPaleoceanography and Paleoclimatology
researchProduct

Tropical Atlantic temperature seasonality at the end of the last interglacial

2015

The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice sheets. These perturbations are crucial for a better understanding of future climate change. The seasonal temperature changes of the tropical ocean, however, which play an important role in seasonal climate extremes such as hurricanes, floods and droughts at the present day, are not well known for this period that led into the last glacial. Here we present a monthly resolved snapshot of reconstructed sea surface temperature in the tropical North Atlantic Ocean for 117.7±0.8 kyr ago, using coral Sr/Ca and δ18O records. W…

geographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ18OOcean currentGeneral Physics and AstronomyGeneral ChemistryTropical Atlantic010502 geochemistry & geophysics01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyArticleSea surface temperatureOceanography13. Climate actionInterglacialClimate model14. Life underwaterGlacial periodIce sheetGeology0105 earth and related environmental sciences
researchProduct

Last interglacial temperature seasonality reconstructed from tropical Atlantic corals

2016

Abstract Reconstructions of last interglacial (LIG, MIS 5e, ∼127–117 ka) climate offer insights into the natural response and variability of the climate system during a period partially analogous to future climate change scenarios. We present well preserved fossil corals (Diploria strigosa) recovered from the southern Caribbean island of Bonaire (Caribbean Netherlands). These have been precisely dated by the 230Th/U-method to between 130 and 120 ka ago. Annual banding of the coral skeleton enabled construction of time windows of monthly resolved strontium/calcium (Sr/Ca) temperature proxy records. In conjunction with a previously published 118 ka coral record, our eight records of up to 37 …

Diploria strigosa010504 meteorology & atmospheric sciencesbiologyCoralSeasonalityTropical Atlantic010502 geochemistry & geophysicsmedicine.diseasebiology.organism_classification01 natural sciencesProxy (climate)Sea surface temperatureGeophysicsOceanography13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyClimatologyInterglacialEarth and Planetary Sciences (miscellaneous)medicineClimate model14. Life underwaterGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
researchProduct

Monthly Bonaire coral Sr/Ca and oxygen isotope data from 118 kyr ago (coral BON-5-D)

2015

The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice sheets. These perturbations are crucial for a better understanding of future climate change. The seasonal temperature changes of the tropical ocean, however, which play an important role in seasonal climate extremes such as hurricanes, floods and droughts at the present day, are not well known for this period that led into the last glacial. Here we present a monthly resolved snapshot of reconstructed sea surface temperature in the tropical North Atlantic Ocean for 117.7±0.8 kyr ago, using coral Sr/Ca and d18O records. W…

CaribClim_Coral_2006Integrierte Analyse zwischeneiszeitlicher Klimadynamik INTERDYNAMIKDrilling/drill rigCalculated see reference(s)Drilling drill rigOptima 3300RPerkin ElmerIntegrierte Analyse zwischeneiszeitlicher Klimadynamik (INTERDYNAMIK)ICP OESMass spectrometer Finnigan MAT 251Diploria strigosaDiploria strigosa δ18OCalculatedEarth System ResearchCenter for Marine Environmental Sciences MARUMsee reference sICP-OES Perkin-Elmer Optima 3300RInternal coral chronologyδ18ODiploria strigosa Strontium/Calcium ratioStrontium Calcium ratioCenter for Marine Environmental Sciences (MARUM)
researchProduct