scholarly journals Continuous vegetation record of the Greater Cape Floristic Region (South Africa) covering the past 300 thousand years (IODP U1479)

2021 ◽  
Author(s):  
Lydie M. Dupont ◽  
Xueqin Zhao ◽  
Chistopher Charles ◽  
J. Tyler Faith ◽  
David Braun

Abstract. The flora of the Greater Cape Floristic Region (GCFR) of South Africa is a biodiversity hotspot of global significance, and its archaeological record has contributed substantially to the understanding of modern human origins. For both reasons, the climate and vegetation history of south-western South Africa is of interest to numerous fields. Currently known paleo-environmental records cover the Holocene, the last glacial-interglacial transition and parts of the last glaciation but do not encompass a full glacial-interglacial cycle. To obtain a continuous vegetation record of the last Pleistocene glacial-interglacial cycles, we studied pollen, spores and micro-charcoal of deep-sea sediments from IODP Site U1479 retrieved from SW of Cape Town. We compare our palynological results of the Pleistocene with previously published results of Pliocene material from the same site. We find that the vegetation of the GCFR, in particular Fynbos and Afrotemperate forest, respond to precessional forcing of climate. The micro-charcoal record confirms the importance of fires in the Fynbos vegetation. Ericaceae-rich and Asteraceae-rich types of Fynbos could extend on the western part of the Palaeo-Agulhas Plain (PAP), which emerged during periods of low sea-level of the Pleistocene.

2022 ◽  
Vol 18 (1) ◽  
pp. 1-21
Author(s):  
Lydie M. Dupont ◽  
Xueqin Zhao ◽  
Christopher Charles ◽  
John Tyler Faith ◽  
David Braun

Abstract. The Greater Cape Floristic Region (GCFR) of South Africa is a biodiversity hotspot of global significance, and its archeological record has substantially contributed to the understanding of modern human origins. For both reasons, the climate and vegetation history of southwestern South Africa is of interest to numerous fields. Currently known paleoenvironmental records cover the Holocene, the last glacial–interglacial transition and parts of the last glaciation but do not encompass a full glacial–interglacial cycle. To obtain a continuous vegetation record of the last Pleistocene glacial–interglacial cycles, we studied pollen, spores and micro-charcoal of deep-sea sediments from IODP Site U1479 retrieved from SW of Cape Town. We compare our palynological results of the Pleistocene with previously published results of Pliocene material from the same site. We find that the vegetation of the GCFR, in particular fynbos and afrotemperate forest, responds to precessional forcing of climate. The micro-charcoal record confirms the importance of fires in the fynbos vegetation. Ericaceae-rich and Asteraceae-rich types of fynbos could extend on the western part of the Paleo-Agulhas Plain (PAP), which emerged during periods of low sea level of the Pleistocene.


2018 ◽  
Vol 91 (2) ◽  
pp. 881-891 ◽  
Author(s):  
J. Andrew Nunnery ◽  
Sherilyn C. Fritz ◽  
Paul A. Baker ◽  
Wout Salenbien

AbstractVarious paleoclimatic records have been used to reconstruct the hydrologic history of the Altiplano, relating this history to past variability of the South American summer monsoon. Prior studies of the southern Altiplano, the location of the world’s largest salt flat, the Salar de Uyuni, and its neighbor, the Salar de Coipasa, generally agree in their reconstructions of the climate history of the past ∼24 ka. Some studies, however, have highly divergent climatic records and interpretations of earlier periods. In this study, lake-level variation was reconstructed from a ∼14-m-long sediment core from the Salar de Coipasa. These sediments span the last ∼40 ka. Lacustrine sediment accumulation was apparently continuous in the basin from ∼40 to 6 ka, with dry or very shallow conditions afterward. The fossil diatom stratigraphy and geochemical data (δ13C, δ15N, %Ca, C/N) indicate fluctuations in lake level from shallow to moderately deep, with the deepest conditions correlative with the Heinrich-1 and Younger Dryas events. The stratigraphy shows a continuous lake of variable depth and salinity during the last glacial maximum and latter stages of Marine Oxygen Isotope Stage 3 and is consistent with environmental inferences and the original chronology of a drill core from Salar de Uyuni.


Blood ◽  
2020 ◽  
Vol 136 (Supplement 1) ◽  
pp. 14-15
Author(s):  
Austin Kulasekararaj ◽  
Jacques Le Roux Malherbe ◽  
Andrew McDonald ◽  
Melanie Cornpropst ◽  
Phil Collis ◽  
...  

INTRODUCTION: PNH, a rare, chronic, life-threatening disease, is characterized by hemolytic anemia due to uncontrolled activity of the complement alternative pathway (AP), bone marrow failure, and thrombosis. Inhibition of C5 by intravenously administered eculizumab and ravulizumab reduces intravascular hemolysis, but PNH red blood cells (RBCs) become opsonized and susceptible to extravascular hemolysis (Risitano et al, Blood 2009). Only approximately half of PNH patients become transfusion independent with eculizumab treatment (Hillmen et al, NEJM 2006). BCX9930 is a potent, selective, orally administered inhibitor of complement factor D. Inhibition of factor D may prevent both intravascular and extravascular hemolysis in PNH. In healthy subjects, BCX9930 showed linear pharmacokinetics and dose-related AP suppression, and was safe and generally well-tolerated over a wide dose range. Here we describe safety and laboratory data establishing proof-of-concept for BCX9930 monotherapy in PNH patients in Study BCX9930-101 (NCT04330534). METHODS: Ongoing Study BCX9930-101 includes an open-label, dose-ranging evaluation of BCX9930 in PNH subjects who may either be naïve to C5 inhibitors (and receive BCX9930 as monotherapy) or have an incomplete treatment response to eculizumab or ravulizumab (with BCX9930 added to existing treatment). Up to 4 sequential cohorts each use a forced titration design for the first 28 days (Figure 1). Subjects enrolled in South Africa can participate in an individualized 48-week extension if they derive benefit at Day 28. Clinical benefit from BCX9930 is evaluated using laboratory monitoring and symptom assessment. Safety and tolerability are evaluated via clinical and laboratory monitoring, causality of adverse events is assessed by investigators, and the study is overseen by an independent Data Monitoring Committee. Data from Cohort 1 through 28 days is reported; data from the extension and subsequent cohorts will be subsequently summarized as available. RESULTS: To date, four C5 inhibitor naïve PNH subjects in South Africa have enrolled in Cohort 1. These subjects had PNH for a median of 4.5 years; 2 subjects had a history of transfusions in the past year; 1 subject each had a history of aplastic anemia or major thrombosis. Pre-treatment lactate dehydrogenase (LDH), total bilirubin, hemoglobin (Hb), reticulocyte count, and RBC PNH Type III clone size ranged from 3.7-11.1 × ULN, 0.61-3.3 mg/dL, 6.1-11.6 g/dL, 0.13-0.29 × 106/µL, and 41.4%-88.6% respectively. Treatment over 28 days with 50 mg twice daily (BID; Days 1-14) and 100 mg BID (Days 15-28) of BCX9930 produced dose-dependent, clinically meaningful improvements across hemolysis biomarkers (Figure 2). Decreases were observed in LDH (4/4), reticulocytes (4/4), and total bilirubin (2/2 subjects with elevated pre-treatment values). Increases were observed in Hb (3/4) and PNH RBC clone size (4/4). One subject showed an initial response to BCX9930 50 mg BID, followed by worsening indicators of hemolysis temporally associated with an upper respiratory tract infection (URTI; onset on Day 7). With an increase in dose to 100 mg BID and resolution of the URTI, LDH and reticulocytes fell and Hb rose. All four subjects reported one or more PNH-associated symptoms, including hemoglobinuria, jaundice, fatigue, erectile dysfunction, headache and abdominal pain, prior to enrollment. With the exception of one subject with persistent hemoglobinuria, all symptoms resolved by Day 28 on BCX9930. Three subjects experienced moderate headache that resolved in < 3 days after initiating BCX9930. One subject developed a rash during treatment with amoxicillin for an URTI; the rash resolved while continuing BCX9930 dosing. One subject on concomitant chronic corticosteroids and azathioprine had an unrelated fatal serious adverse event of disseminated varicella during the study extension. Based on review of safety data, Cohort 2 opened at doses of 200 mg BID and 400 mg BID and, in the 3 subjects who continued into the extension, the dose was titrated to ≥ 200 mg BID. CONCLUSIONS: Oral BCX9930 elicited rapid changes in laboratory parameters indicative of reduced hemolysis and clinical benefit and was safe and generally well-tolerated over a 28-day dosing interval. These interim results establish proof of concept for monotherapy with BCX9930 in the treatment of C5-inhibitor naïve PNH patients and support evaluation of higher doses. Disclosures Kulasekararaj: Alexion:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees, Other: Travel grants, Speakers Bureau;Ra Pharma:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees, Other: Travel grants, Speakers Bureau;BioCryst Pharmaceuticals, Inc.:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees;Apellis:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees, Other: Travel grants, Speakers Bureau;Roche:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees, Speakers Bureau;Novartis:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees, Other: Travel grants, Speakers Bureau;Celgene:Consultancy, Honoraria, Membership on an entity's Board of Directors or advisory committees, Other: Travel grants, Speakers Bureau.Malherbe:Key Oncologics:Honoraria, Other: Conference sponsor;Novartis:Other: Conference sponsor;Astellas:Honoraria, Other: Conference sponsor;Takeda:Consultancy;Acino:Honoraria;Shire:Other: Conference sponsor;BioCryst Pharmaceuticals, Inc.:Consultancy;Janssen:Consultancy, Honoraria, Other: Conference sponsor;Roche:Honoraria, Other: Conference sponsor.McDonald:venetoclax advisory board in South Africa (in CLL context):Consultancy;Alberts Cellular Therapy:Current Employment.Cornpropst:BioCryst Pharmaceuticals, Inc.:Current Employment.Collis:BioCryst Pharmaceuticals, Inc.:Current Employment.Davidson:BioCryst Pharmaceuticals, Inc.:Current Employment.Chen:BioCryst Pharmaceuticals, Inc.:Current Employment.Tower:BioCryst Pharmaceuticals, Inc.:Current Employment.Gesty-Palmer:BioCryst Pharmaceuticals, Inc.:Current equity holder in publicly-traded company, Ended employment in the past 24 months.Sheridan:BioCryst Pharmaceuticals, Inc.:Current Employment.Risitano:Alexion:Consultancy, Membership on an entity's Board of Directors or advisory committees, Research Funding, Speakers Bureau;Alnylam:Research Funding;Novartis:Membership on an entity's Board of Directors or advisory committees, Research Funding, Speakers Bureau;Pfizer:Speakers Bureau;Achillion:Membership on an entity's Board of Directors or advisory committees;Apellis:Membership on an entity's Board of Directors or advisory committees, Speakers Bureau;Biocryst:Membership on an entity's Board of Directors or advisory committees;RA pharma:Research Funding;Amyndas:Consultancy;Samsung:Membership on an entity's Board of Directors or advisory committees;Roche:Membership on an entity's Board of Directors or advisory committees;Jazz:Speakers Bureau.


2019 ◽  
Author(s):  
S. V. Dryomov ◽  
A. M. Nazhmidenova ◽  
E. B. Starikovskaya ◽  
S. A. Shalaurova ◽  
N. Rohland ◽  
...  

AbstractThe Central Siberian Plateau was last geographic area in Eurasia to become habitable by modern humans after the Last Glacial Maximum (LGM). Through comprehensive mitochondrial DNA genomes retained in indigenous Siberian populations, the Ket, Tofalar, and Todzhi - we explored genetic links between the Yenisei-Sayan region and Northeast Eurasia over the last 10,000 years. Accordingly, we generated 218 new complete mtDNA sequences and placed them into compound phylogenies along with 7 newly obtained and 70 published ancient mt genomes. Our findings reflect the origins and expansion history of mtDNA lineages that evolved in South-Central Siberia, as well as multiple phases of connections between this region and distant parts of Eurasia. Our result illustrates the importance of jointly sampling modern and prehistoric specimens to fully measure the past genetic diversity and to reconstruct the process of peopling of the high latitudes of the Siberian subcontinent.


1992 ◽  
Vol 37 (2) ◽  
pp. 203-213 ◽  
Author(s):  
A.S. Talma ◽  
John C. Vogel

AbstractAn oxygen isotope temperature record over a large part of the past 30,000 yr has been obtained for the southern Cape Province of South Africa by combining data on the isotopic composition of a stalagmite from a deep cave with that of a confined groundwater aquifer in the same region. Results show that temperatures during the last glacial maximum were on average about 6°C lower than those today, with peaks up to 7°C lower. A detailed analysis of the past 5000 yr suggests multiple fluctuations, with generally lower temperatures (1–2°C) around 4500 and 3000 yr B.P. The carbon isotopic composition of the stalagmite indicates significant vegetation changes between the late Pleistocene and today, and also during the second half of the Holocene.


The Holocene ◽  
2020 ◽  
Vol 30 (6) ◽  
pp. 888-904
Author(s):  
Emilie Gouriveau ◽  
Pascale Ruffaldi ◽  
Loïc Duchamp ◽  
Vincent Robin ◽  
Annik Schnitzler ◽  
...  

Palynological data from the Northern Vosges Mountains (NVM) are very rare, unlike for the Southern and Central Vosges Mountains, where the past vegetation history is relatively well known. As a consequence, the beginning of human activities has never been clearly identified and dated in the NVM. In order to reconstruct the evolution of vegetation in this region, multiproxy studies (pollen, non-pollen palynomorphs, sedimentological and geochemical analyses) were conducted in two peatlands. Overall, the results, extending from about 9500 cal. BP to recent times, show a classical vegetation succession with local particularities resulting from human activities. In the La Horn peatland, a strong human impact related to pastoralism is attested from the late Bronze Age onwards. The second phase of human occupation, mainly characterized by crop cultures, begins during the Hallstatt period. The geochemical results (x-ray fluorescence) also highlight the presence of metallic elements, which, combined with significant quantities of carbonized particles, point to potential metal working. In the Kobert-Haut peatland, human occupation began much later (1500 cal. BP), but lasted from the Gallo-Roman period to the beginning of the Modern Period. Unlike for the vegetation history of the rest of the Vosges, Pinus remains a prevailing taxon throughout the Holocene in the NVM. Another particularity is the early establishment of Picea, long before the 18th to 19th century plantations.


Literator ◽  
1994 ◽  
Vol 15 (2) ◽  
pp. 19-34
Author(s):  
W. A.M. Carstens

This article focuses on views expressed in newspaper articles and in letters to the editor about the future of Afrikaans in a new political dispensation. It seems as if people do not believe that despite the constitutional assurances of November 1993 - Afrikaans will be able to maintain its present status as one of the official languages of South Africa as the mistakes of the past are constantly being thrown into its face. There have been signs in the business community (for example by Toyota, Coca-Cola, BMW, SA Breweries) and in the political arena that English, rather than Afrikaans, is the favoured language. The views expressed in the articles and letters indicate that the Afrikaans community will not accept this attitude and that a new struggle for language rights (especially those of Afrikaans in the light of the history of Afrikaans) could be the result. This struggle could according to one letter writer - have serious consequences for peace in the country after the assumption of power by a new government will come to power after April 27 1994.


2018 ◽  
Vol 91 (2) ◽  
pp. 848-860 ◽  
Author(s):  
J. Tyler Faith ◽  
Brian M. Chase ◽  
D. Margaret Avery

AbstractThe southern Cape of South Africa is important to understanding regional climate because it straddles the transition between the winter and summer rainfall zones. We examine late Quaternary changes in rainfall seasonality and aridity through analysis of micromammal assemblages from three sites: Boomplaas Cave and Nelson Bay Cave in the aseasonal rainfall zone and Byneskranskop 1 in the winter rainfall zone. Our interpretation is based on analysis of 123 modern micromammal assemblages accumulated by barn owls (Tyto alba), which empirically links species composition to climate. The Pleistocene record (∼65 to 12 ka) from Boomplaas Cave, together with the last glacial maximum (LGM) samples from Nelson Bay Cave, indicates enhanced winter rainfall, especially during the LGM. Boomplaas Cave documents progressive aridification from the LGM to the earliest Holocene, followed by a return to moderately humid conditions through the Holocene. Byneskranskop 1 indicates a dominance of winter rains over the last 17 ka and a shift from an arid middle Holocene to a humid later Holocene. Agreement between the micromammal record and other local and regional proxies reinforces the potential of southern African micromammal assemblages as paleoclimate indicators.


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