TY  - JOUR
A1  - Vogt-Vincent, Noam
A1  - Lippold, Jörg
A1  - Kaboth-Bahr, Stefanie
A1  - Blaser, Patrick
T1  - Ice-rafted debris as a source of non-conservative behaviour for the epsilon Nd palaeotracer
BT  - insights from a simple model
JF  - Geo-marine letters : an international journal of marine geology
N2  - Neodymium isotopic composition (epsilon Nd) has enjoyed widespread use as a palaeotracer, principally because it behaves quasi-conservatively in the modern ocean. However, recent bottom water epsilon Nd reconstructions from the eastern North Atlantic are difficult to interpret under assumptions of conservative behaviour. The observation that this apparent departure from conservative behaviour increases with enhanced ice-rafted debris (IRD) fluxes has resulted in the suggestion that IRD leads to the overprinting of bottom water epsilon Nd through reversible scavenging. In this study, a simple water column model successfully reproduces epsilon Nd reconstructions from the eastern North Atlantic at the Last Glacial Maximum and Heinrich Stadial 1, and demonstrates that the changes in scavenging intensity required for good model-data fit is in good agreement with changes in the observed IRD flux. Although uncertainties in model parameters preclude a more definitive conclusion, the results indicate that the suggestion of IRD as a source of non-conservative behaviour in the epsilon Nd tracer is reasonable and that further research into the fundamental chemistry underlying the marine neodymium cycle is necessary to increase confidence in assumptions of conservative epsilon Nd behaviour in the past.
KW  - Neodymium isotopes
KW  - epsilon Nd
KW  - ice-rafted debris
KW  - IRD
KW  - last glacial
KW  - maximum
KW  - LGM
KW  - Heinrich event
KW  - Palaeoceanography
KW  - Paleoceanography
KW  - model
KW  - reversible scavenging
KW  - conservative
KW  - ocean circulation
KW  - atlantic
KW  - meridional overturning circulation
KW  - geochemical cycling
Y1  - 2020
U6  - https://doi.org/10.1007/s00367-020-00643-x
SN  - 0276-0460
SN  - 1432-1157
VL  - 40
IS  - 3
SP  - 325
EP  - 340
PB  - Springer
CY  - Berlin
ER  - 
TY  - JOUR
A1  - Reschke, Maria
A1  - Kröner, Igor
A1  - Laepple, Thomas
T1  - Testing the consistency of Holocene and Last Glacial Maximum spatial correlations in temperature proxy records
JF  - Journal of quaternary science : JQS
N2  - Holocene temperature proxy records are commonly used in quantitative synthesis and model-data comparisons. However, comparing correlations between time series from records collected in proximity to one another with the expected correlations based on climate model simulations indicates either regional or noisy climate signals in Holocene temperature proxy records. In this study, we evaluate the consistency of spatial correlations present in Holocene proxy records with those found in data from the Last Glacial Maximum (LGM). Specifically, we predict correlations expected in LGM proxy records if the only difference to Holocene correlations would be due to more time uncertainty and more climate variability in the LGM. We compare this simple prediction to the actual correlation structure in the LGM proxy records. We found that time series data of ice-core stable isotope records and planktonic foraminifera Mg/Ca ratios were consistent between the Holocene and LGM periods, while time series of Uk'37 proxy records were not as we found no correlation between nearby LGM records. Our results support the finding of highly regional or noisy marine proxy records in the compilation analysed here and suggest the need for further studies on the role of climate proxies and the processes of climate signal recording and preservation.
KW  - Holocene
KW  - LGM
KW  - spatial correlation
KW  - temperature
KW  - Uk'37
Y1  - 2020
U6  - https://doi.org/10.1002/jqs.3245
SN  - 0267-8179
SN  - 1099-1417
VL  - 36
IS  - 1
SP  - 20
EP  - 28
PB  - Wiley
CY  - New York
ER  -