Benthic-Pelagic state changes in the primary trophic level of an ancient tropical lake

被引:4
作者
Ageli, Mariam K. [1 ]
Hamilton, Paul B. [2 ]
Bramburger, Andrew J. [3 ]
Weidman, R. Paul [1 ]
Song, Zhuoyan [1 ]
Russell, James [4 ]
Vogel, Hendrik [5 ,6 ]
Bijaksana, Satria [7 ]
Haffner, G. Douglas [1 ]
机构
[1] Univ Windsor, Great Lakes Inst Environm Res, Windsor, ON N9B 3P4, Canada
[2] Canadian Museum Nat, Res & Collect Div, POB 3443, Ottawa, ON K1P 6P4, Canada
[3] Environm & Climate Change Canada, Watershed Hydrol & Ecol Res Div, 867 Lakeshore Rd, Burlington, ON L7S 1A1, Canada
[4] Brown Univ, Dept Earth Environm & Planetary Sci, 324 Brook St, Providence, RI 02912 USA
[5] Univ Bern, Inst Geol Sci, CH-13 Bern, Switzerland
[6] Univ Bern, Oeschger Ctr Climate Change Res, CH-13 Bern, Switzerland
[7] Inst Teknol Bandung, Fac Min & Petr Engn, Bandung 40132, Indonesia
基金
加拿大自然科学与工程研究理事会; 瑞士国家科学基金会; 美国国家科学基金会;
关键词
Paleolimnology; Ancient lakes; Evolution; Diatoms; Primary production; Lake Towuti; ADAPTIVE RADIATION; SULAWESI ISLAND; MALILI LAKES; SAILFIN SILVERSIDES; RELATIVE ABUNDANCE; DIATOM RECORD; COMMUNITY; TOWUTI; MATANO; INDONESIA;
D O I
10.1016/j.palaeo.2022.110937
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Many large, ancient lakes support primarily planktonic-driven food webs. In contrast, the lowest trophic levels of the Malili Lakes of Sulawesi Island, Indonesia are dominated by benthic diatom communities composed mainly of endemic species. Centric diatoms are not observed in the current diatom assemblage and pennate pelagic species are rare. Using two deep drill-cores from Lake Towuti, we investigated whether the lake has always been dominated by benthic primary production. Despite the ultra-oligotrophic conditions observed in the lake today, we observed state changes characterized by productive planktonic communities and less productive, benthic-dominated diatom assemblages. Two periods of planktonic production, each lasting approximately 50 kyr, were dominated by a complex mixture of Aulacoseira spp., with valve densities > 1.0 x 10(9) valves/g with a maximum biovolume of 3.5 x 10(12) mu m(3)/g. A similar planktonic assemblage was observed at much lower abundances (< 107valves/g) in the deeper sediments (> 1 Ma), during the earliest stages of lake formation. Two periods of increased benthic primary production of approximately ~11 kyr in duration, originating from the littoral zone of the lake, were also observed, one between the two planktonic phases and one above the last planktonic maxima. The benthic periods were dominated by Cymbopleura spp., with valve densities of approximately 2.0 x 10(8) valves/g and a maximum biovolume of 1.2 x 10(11) mu m(3)/g. Nonmetric multidimensional scaling analysis of sediment chemistry revealed that the benthic and pelagic states clustered with distinct chemical environments. The benthic phases were associated with well-mixed conditions in the lake whereas the planktonic phases were related to rapidly reoccurring water column mixing followed by intense stratification that generate nutrient recycling events. We conclude that lake mixing and nutrient cycling regimes regulated, in part, the switch between benthic and pelagic states in Lake Towuti.
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页数:11
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