| 1. |
- Palmer, Jonathan G., et al.
(författare)
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Changes in El Niño – Southern Oscillation (ENSO) conditions during the Greenland Stadial 1 (GS-1) chronozone revealed by New Zealand tree-rings
- 2016
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Ingår i: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791. ; 153, s. 139-155
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Tidskriftsartikel (refereegranskat)abstract
- The warming trend at the end of the last glacial was disrupted by rapid cooling clearly identified in Greenland (Greenland Stadial 1 or GS-1) and Europe (Younger Dryas Stadial or YD). This reversal to glacial-like conditions is one of the best known examples of abrupt change but the exact timing and global spatial extent remain uncertain. Whilst the wider Atlantic region has a network of high-resolution proxy records spanning GS-1, the Pacific Ocean suffers from a scarcity of sub-decadally resolved sequences. Here we report the results from an investigation into a tree-ring chronology from northern New Zealand aimed at addressing the paucity of data. The conifer tree species kauri (Agathis australis) is known from contemporary studies to be sensitive to regional climate changes. An analysis of a ‘historic’ 452-year kauri chronology confirms a tropical-Pacific teleconnection via the El Niño – Southern Oscillation (ENSO). We then focus our study on a 1010-year sub-fossil kauri chronology that has been precisely dated by comprehensive radiocarbon dating and contains a striking ring-width downturn between ∼12,500 and 12,380 cal BP within GS-1. Wavelet analysis shows a marked increase in ENSO-like periodicities occurring after the downturn event. Comparison to low- and mid-latitude Pacific records suggests a coherency with ENSO and Southern Hemisphere atmospheric circulation change during this period. The driver(s) for this climate event remain unclear but may be related to solar changes that subsequently led to establishment and/or increased expression of ENSO across the mid-latitudes of the Pacific, seemingly independent of the Atlantic and polar regions.
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| 2. |
- Turney, Chris S M, et al.
(författare)
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High-precision dating and correlation of ice, marine and terrestrial sequences spanning Heinrich Event 3 : Testing mechanisms of interhemispheric change using New Zealand ancient kauri (Agathis australis)
- 2016
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Ingår i: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791. ; 137, s. 126-134
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Tidskriftsartikel (refereegranskat)abstract
- Robustly testing hypotheses of geographic synchroneity of abrupt and extreme change during the late Pleistocene (60,000 to 11,650 years ago) requires a level of chronological precision often lacking in ice, marine and terrestrial sequences. Here we report a bidecadally-resolved New Zealand kauri (Agathis australis) tree-ring sequence spanning two millennia that preserves a record of atmospheric radiocarbon (14C) during ice-rafted debris event Heinrich Event 3 (HE3) in the North Atlantic and Antarctic Isotope Maximum 4 (AIM4) in the Southern Hemisphere. Using 14C in the marine Cariaco Basin and 10Be preserved in Greenland ice, the kauri 14C sequence allows us to precisely align sequences across this period. We observe no significant difference between atmospheric and marine 14C records during HE3, suggesting no stratification of surface waters and collapse in Atlantic Meridional Overturning Circulation (AMOC). Instead our results support recent evidence for a weakened AMOC across at least two millennia of the glacial period. Our work adds to a growing body of literature confirming that Heinrich events are not the cause of stadial cooling and suggests changes in the AMOC were not the primary driver of antiphase temperature trends between the hemispheres. Decadally-resolved 14C in ancient kauri offers a powerful new (and complementary) approach to polar ice core CH4 alignment for testing hypotheses of abrupt and extreme climate change.
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| 3. |
- Turney, Chris S M, et al.
(författare)
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Rapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial
- 2017
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Ingår i: Nature Communications. - : Springer Science and Business Media LLC. - 2041-1723. ; 8:1
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Tidskriftsartikel (refereegranskat)abstract
- Contrasting Greenland and Antarctic temperatures during the last glacial period (115,000 to 11,650 years ago) are thought to have been driven by imbalances in the rates of formation of North Atlantic and Antarctic Deep Water (the 'bipolar seesaw'). Here we exploit a bidecadally resolved 14C data set obtained from New Zealand kauri (Agathis australis) to undertake high-precision alignment of key climate data sets spanning iceberg-rafted debris event Heinrich 3 and Greenland Interstadial (GI) 5.1 in the North Atlantic (~30,400 to 28,400 years ago). We observe no divergence between the kauri and Atlantic marine sediment 14C data sets, implying limited changes in deep water formation. However, a Southern Ocean (Atlantic-sector) iceberg rafted debris event appears to have occurred synchronously with GI-5.1 warming and decreased precipitation over the western equatorial Pacific and Atlantic. An ensemble of transient meltwater simulations shows that Antarctic-sourced salinity anomalies can generate climate changes that are propagated globally via an atmospheric Rossby wave train.
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| 4. |
- Löwenmark, Thyra, 1995-
(författare)
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Gut microbiota in colorectal cancer : The importance of Parvimonas micra
- 2024
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Doktorsavhandling (övrigt vetenskapligt/konstnärligt)abstract
- Colorectal cancer (CRC) is a heterogenous disease consisting of multiple molecular subtypes, each of which has diverse treatment responses and prognoses. The importance of the gut microbiota in CRC development and progression has undergone increasing recognition in recent years, with a structural segregation in terms of microbial composition between CRC patients and healthy controls. However, many questions remain before a full understanding of the impact of the gut microbiota on CRC is reached. The overall aim of this thesis was to explore the role of gut microbes in CRC, including their potential as CRC biomarkers and associations with clinicopathological, immunological, and molecular traits of CRC. A particular focus was the CRC-associated oral pathogen Parvimonas micra.To investigate faecal microbiota as a potential biomarker for CRC, we studied the presence of specific bacteria in faeces from CRC patients and controls using qPCR. We found higher levels of P. micra in faecal samples from CRC patients than from control patients. A test for high levels of P. micra was able to identify CRC with a specificity of 87.3% and a sensitivity of 60.5%. Adding the oral pathogen Fusobacterium nucleatum, colibactin-producing bacteria, and faecal haemoglobin to the test enhanced its sensitivity.We further aimed to explore the associations of P. micra and F. nucleatum with molecular subtypes of CRC and the tumour immune response. The levels of P. micra and F. nucleatum, as analysed by qPCR in both faeces and tumour tissue from CRC patients, were found to be positively correlated. High levels of intratumoural P. micra and F. nucleatum were associated with tumours of the microsatellite instable subtype and BRAF-mutated tumours. For F. nucleatum, an additional association with right-sided tumours was found. Moreover, both P. micra and F. nucleatum in tumour tissue were associated with the immune-activated consensus molecular subtype (CMS) 1 subtype of CRC. In line with this finding, we found novel associations between intratumoural P. micra and specific immune traits, which were evaluated by flow cytometry, indicating an active immune response in CRC. These results were further confirmed using transcriptomics. However, no associations with specific immune traits were found for F. nucleatum.We also investigated associations between faecal and intratumoural levels of P. micra and F. nucleatum and survival in CRC patients. CRC patients with high levels of intratumoural P. micra and F. nucleatum showed reduced five-year cancer-specific survival. This association remained significant for P. micra in multivariable analysis. No associations with cancer-specific survival were found for levels of P. micra and F. nucleatum in faeces.To investigate the faecal microbial landscape of CRC patients on a larger scale, we used 16S rRNA sequencing. Network analysis revealed a cluster of associated bacteria, including P. micra and F. nucleatum, as well as other CRC-related pathogens such as Bacteroides fragilis, Peptostreptococcus stomatitis, and Porphyromonas spp. Furthermore, beta-diversity analysis indicated a significantly different gut microbial composition depending on tumour location and microsatellite instability status. Interestingly, three of the six annotated species most strongly associated with microsatellite instable tumours were also present in the cluster: P. micra, F. nucleatum, and P. stomatis.In conclusion, our results suggest P. micra as a putative candidate for a future non-invasive microbial test panel for detection of CRC. Moreover, our results indicate that intratumoural P. micra and F. nucleatum are associated with immune-active subtypes of CRC, including microsatellite instable tumours and tumours of the CMS1 subtype, as well as decreased patient survival. Furthermore, P. micra and F. nucleatum were found to be associated with a cluster of other CRC-related oral pathogens. An improved understanding of the role of the gut microbiota in tumour progression may lead to the identification of important biomarkers for CRC disease and outcome, as well as potential targets for future therapy.
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| 5. |
- Staff, Richard A., et al.
(författare)
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Reconciling the Greenland ice-core and radiocarbon timescales through the Laschamp geomagnetic excursion
- 2019
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Ingår i: Earth and Planetary Science Letters. - : Elsevier BV. - 0012-821X. ; 520, s. 1-9
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Tidskriftsartikel (refereegranskat)abstract
- Cosmogenic radionuclides, such as 10Be and 14C, share a common production signal, with their formation in the Earth's upper atmosphere modulated by changes to the geomagnetic field, as well as variations in the intensity of the solar wind. Here, we use this common production signal to compare between the radiocarbon (IntCal)and Greenland ice-core (GICC05)timescales, utilising the most pronounced cosmogenic production peak of the last 100,000 years – that associated with the Laschamp geomagnetic excursion circa 41,000 years ago. We present 54 new 14C measurements from a peat core (‘TP-2005’)from Tenaghi Philippon, NE Greece, contiguously spanning between circa 47,300 and 39,600 cal. BP, demonstrating a distinctive tripartite structure in the build up to the principal Laschamp production maximum that is not present in the consensus IntCal13 calibration curve. This is the first time that a continuous, non-reservoir corrected 14C dataset has been generated over such a long time span for this, the oldest portion of the radiocarbon timescale. This period is critical for both palaeoenvironmental and archaeological applications, with the replacement of Neanderthals by anatomically modern humans in Europe around this time. By placing our Tenaghi Philippon 14C dataset on to the Hulu Cave U-series timescale of Cheng et al. (2018)via Bayesian statistical modelling, the comparison of TP-2005 14C with Greenland 10Be fluxes also implicitly relates the underlying U-series and GICC05 timescales themselves. This comparison suggests that whilst these two timescales are broadly coherent, the IntCal13 timescale contains erroneous structure circa 40,000 cal. BP.
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