Taxonomic study ofBarbus neumayeriandBarbus pellegrinifrom the Lake Kivu-Lake Edward region, East Africa

2013 ◽  
Vol 51 (2) ◽  
pp. 300-306
Author(s):  
Chrisestom Mwatete Mlewa
2020 ◽  
Vol 532 ◽  
pp. 119374
Author(s):  
Fabian Bärenbold ◽  
Martin Schmid ◽  
Matthias S. Brennwald ◽  
Rolf Kipfer

1972 ◽  
Vol 7 (1) ◽  
Author(s):  
E.T. Degens ◽  
H. Okada ◽  
S. Honjo ◽  
J.C. Hathaway
Keyword(s):  

2016 ◽  
Vol 79 (2) ◽  
pp. 209-218 ◽  
Author(s):  
Fleur A. E. Roland ◽  
François Darchambeau ◽  
Cédric Morana ◽  
Alberto V. Borges

2016 ◽  
Vol 61 (4) ◽  
pp. 1424-1437 ◽  
Author(s):  
Cédric Morana ◽  
Fleur A. E. Roland ◽  
Sean A. Crowe ◽  
Marc Llirós ◽  
Alberto V. Borges ◽  
...  

Sedimentology ◽  
1974 ◽  
Vol 21 (1) ◽  
pp. 163-170 ◽  
Author(s):  
PETER STOFFERS ◽  
REINHARD FISCHBECK
Keyword(s):  

2017 ◽  
Vol 89 (1) ◽  
pp. 7-20 ◽  
Author(s):  
Sarah J. Ivory ◽  
James Russell

AbstractIn Africa, the early Holocene was characterized by wetter, warmer conditions than today, followed by rapid aridification at ~5.2 ka. However, a lack of lowland vegetation records has prevented a detailed evaluation of forest response to Holocene climate change. Additionally, although modern vegetation communities are linked to human disturbance, few studies have addressed how prehistoric human activities helped engineer the character of modern African ecosystems. Understanding the architecture of lowland and highland forests is important to prevent further degradation from climate/land-use change. We present an 11,000 yr fossil pollen record from Lake Edward, Uganda. We show that Guineo-Congolian forests dominated the highlands and lowlands in equatorial East Africa in the early Holocene, highlighting the importance of rainfall and temperature in controlling forest communities. These forests remained until ~5.2 ka, when the climate became drier. The lacustrine ecosystem response to aridification was abrupt; however, forest decreased gradually, replaced by deciduous woodlands. Woodlands dominated until after an arid period at 2 ka; however, forest did not recover. Increased disturbance indicators and grasses suggest that the arrival of Iron Age people resulted in the modern fire-tolerant vegetation. Although late Holocene climate played a role in vegetation opening, the modern ecosystem architecture in East Africa is linked to early human activities.


2014 ◽  
Vol 11 (12) ◽  
pp. 17227-17254 ◽  
Author(s):  
C. Morana ◽  
F. Darchambeau ◽  
F. A. E. Roland ◽  
A. V. Borges ◽  
F. Muvundja ◽  
...  

Abstract. During this study, we investigated the seasonal variability of the concentration and the stable isotope composition of several inorganic and organic matter reservoirs in the large, oligotrophic and deep tropical Lake Kivu (East Africa). Data were acquired during one year at a fornightly temporal resolution. The δ13C signature of the dissolved inorganic carbon (DIC) increased linearly with time during the rainy season, then suddenly decreased during the dry season due to vertical mixing with δ13C-depleted DIC waters. This pattern reflects the net autotrophic status of the mixed layer of Lake Kivu, contrary to the common observation that oligotrophic aquatic ecosystems tend to be net heterotrophic. The δ13C signature of the particulate organic carbon pool (POC) revealed the presence of a consistently abundant methanotrophic biomass in the oxycline throughout the year. We also noticed a seasonal shift during the dry season toward higher values in the δ15N of particulate nitrogen (PN) in the mixed layer and δ15N-PN was significantly related to the contribution of cyanobacteria to the phytoplankton assemblage, suggesting that rainy season conditions could be more favourable to atmospheric nitrogen-fixing cyanobacteria. Finally, zooplankton were slightly enriched in δ13C compared to the autochtonous POC pool, and the δ15N signature of zooplankton followed well the seasonal variability in δ15N-PN, being consistently 3.0 ± 1.1‰ heavier than the PN pool. Together, δ13C and δ15N analysis suggests that zooplankton directly incorporate algal-derived organic matter in their biomass, and they would rely almost exclusively on this source of organic matter throughout the year in general agreement with the very low allochthonous organic matter inputs from rivers in Lake Kivu.


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