Skip to main content

Advertisement

Log in

Delivery and deposition of organic matter in surface sediments of Lagoa do Caçó (Brazil)

  • Original paper
  • Published:
Journal of Paleolimnology Aims and scope Submit manuscript

Abstract

Elemental and isotopic compositions of organic matter in surficial sediments from five transects across Lagoa do Caçó (Brazil) were analyzed to identify the depth-related processes that affect the production and deposition of sedimentary organic matter in this shallow tropical lake. Each of four transverse transects began at a margin dominated by aquatic macrophytes (Eleocharis), crossed the central deep part of the lake, and terminated in the opposite, macrophyte-dominated margin. In each transect, TOC concentrations, C/N ratios, and δ13C values decreased between 0 and 4 m, whereas δ15N values increased. The variables remained stable in sediment from 4 m water depth to the center of the lake at 10 m. The depth-related patterns reflect differences in both the delivery and the deposition of organic matter in the lake. Organic matter is produced in abundance in the marginal area by emersed and submerged macrophyte vegetation that diminishes with depth and disappears at 4 meters. After the disappearance of macrophytes, organic matter is produced at low rates principally by open-lake phytoplankton. Drawdown of dissolved oxygen is high in the lake margins, but it is low in the oligotrophic open waters of the lake. Preservation of organic matter is consequently better in sediments of the lake margins than in deep waters. The depth-related pattern of organic matter delivery and deposition in the sediments of Lagoa do Caçó, in which water levels are sensitive to groundwater fluctuations, shows that the elemental and isotopic compositions of sediment organic matter can provide a record of changes in the paleohydrology of this and other similar shallow lake systems.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6

Similar content being viewed by others

References

  • Boon PI, Bunn SE (1994) Variations in the stable isotope composition of aquatic plants and their implications for food web analysis. Aquat Bot 48:99–108

    Article  Google Scholar 

  • Brenner M, Whitmore TJ, Curtis JH, Hodell DA, Schelske CL (1999) Stable isotope (δ13C and δ15N) signatures of sedimented organic matter as indicators of historic lake trophic state. J Paleolimnol 22:205–221

    Article  Google Scholar 

  • Cardoso AGA (2004) Reconstrução paleoambiental na Lagoa do Caço (Maranhão–Brasil) durante os ultimos 21.000 anos A.P. por marcadores e processos inorgânicos sedimentares. PhD dissertation, Department of Geochemistry, Fluminense Federal University, 127 pp, unpublished PhD dissertation

  • Dellamano-Oliveira MJ, Senna PAC, Taniguchi GM (2003) Limnological characteristics and seasonal changes in density and diversity of the phytoplanktonic community at the Caçó Pond, Maranhão State, Brazil. Braz Arch Biol Tech 46:641–651

    Google Scholar 

  • Fellerhoff C, Voss M, Wantzen KM (2003) Stable carbon and nitrogen isotope signatures of decomposing tropical macrophytes. Aquat Ecol 37:361–375

    Article  Google Scholar 

  • Hassan KM, Swinehart JB, Spalding RF (1997) Evidence for holocene environmental change from C/N ratios and δ13C and δ15N values in Swan Lake sediments, western Sand Hills, Nebraska. J Paleolimnol 18:121–130

    Article  Google Scholar 

  • Jacob J, Disnar J-R, Boussafir M, Ledru M-P, Albuquerque ALS, Sifeddine A, Turcq B (2004a) Onocerane attests to dry climatic events during the quaternary in the tropics. Org Geochem 35:289–297

    Article  Google Scholar 

  • Jacob J, Disnar J-R, Boussafir M, Ledru M-P, Sifeddine A, Turcq B, Albuquerque ALS (2004b) Major environmental changes recorded by lacustrine sedimentary organic matter since the last glacial maximum near the equator (Lagoa do Caçó, NE Brazil). Palaeogeogr Palaeoclimatol Palaeoecol 205:183–197

    Article  Google Scholar 

  • Jacob J, Disnar J-R, Boussafir M, Ledru M-P, Albuquerque ALS, Sifeddine A, Turcq B (2007a) Contrasted distributions of triterpenes derivatives in the sediments of Lake Caçó reflect paleoenvironmental changes during the last 20, 000 yrs in NE Brazil. Org Geochem 38:180–197

    Article  Google Scholar 

  • Jacob J, Huang Y, Disnar J-R, Sifeddine A, Boussafir M, Albuquerque ALS, Turcq B (2007b) Paleohydrological changes during the last deglaciation in Northern Brazil. Quat Sci Rev 26:1004–1015

    Article  Google Scholar 

  • Jolliffe IT (2002) Principal component analysis, 2nd edn. Springer, NY

    Google Scholar 

  • Kaushal S, Binford MW (1999) Relationship between C: N ratios of lake sediments, organic matter sources, and historical deforestation of Lake Pleasant, Massachusetts, USA. J Paleolimnol 22:439–442

    Article  Google Scholar 

  • Krishnamurthy RV, Bhattacharya SK, Kusumgar S (1986) Palaeoclimatic changes deduced from 13C/12C and C/N ratios of Karewa lake sediments. Nature 323:150–152

    Article  Google Scholar 

  • Ledru M-P, Cordeiro RC, Dominguez JML, Martin L, Mourguiart P, Sifeddine A, Turcq B (2001) Late-glacial cooling in Amazonia inferred from pollen at Lagoa do Caçó, northern Brazil. Quat Res 55:47–56

    Article  Google Scholar 

  • Ledru M-P, Mourguiart P, Ceccantini G, Turcq B, Sifeddine A (2002) Tropical climates in the game of two hemispheres revealed by abrupt climate change. Geology 30:275–278

    Article  Google Scholar 

  • Ledru M-P, Ceccantini G, Gouveia SEM, Lopez-Sáez JA, Pessenda LCR, Ribeiro AS (2006) Millennial-scale climate and vegetation changes in a northern Cerrado (Northeast Brazil) since the Last Glacial Maximum. Quat Sc Rev 25:1110–1126

    Article  Google Scholar 

  • Meyers PA (1994) Preservation of elemental and isotopic source identification of sedimentary organic matter. Chem Geol 114:289–302

    Article  Google Scholar 

  • Meyers PA, Teranes JL (2001) Sediment organic matter. In: Last WM, Smol JP (eds) Tracking environmental changes using lake sediments—volume II: physical and chemical techniques. Kluwer, Dordrecht, pp 239–269

    Google Scholar 

  • Nascimento LR, Sifeddine A, Torgan LC, Albuquerque ALS (2010) Diatom assemblage in a tropical lake of northeastern Brazil. Braz Arch Biol Tech 53:241–248

    Article  Google Scholar 

  • Routh J, Choudhary P, Meyers PA, Kumar B (2009) A sediment record of recent nutrient loading and trophic state change in Lake Norrviken, Sweden. J Paleolimnol 42:325–341

    Article  Google Scholar 

  • Sifeddine A, Albuquerque ALS, Ledru M-P, Turcq B, Knoppers BA, Martin L, Mello WZD, Passenau H, Dominquez JML, Cordeiro RC, Abrão JJ, Bittencourt ACSP (2003) A 21,000 cal years paleoclimate change in Caçó Lake, northern Brazil: evidence from sedimentary and pollen records. Palaeogeogr Palaeoclimatol Palaeoecol 189:25–34

    Article  Google Scholar 

  • Sifeddine A, Wirrmann D, Albuquerque ALS, Turcq B, Cordeiro RC, Gurgel MHC, Abrão JJ (2004) Bulk composition of sedimentary organic matter palaeoenvironmental reconstructions: examples from the tropical belt of South America and Africa. Palaeogeogr Palaeoclimatol Palaeoecol 214:41–53

    Google Scholar 

  • Talbot MR, Laerdal T (2000) The late pleistocene-holocene palaeolimnology of Lake Victoria, East Africa, based upon elemental and isotopic analyses of sedimentary organic matter. J Paleolimnol 23:141–164

    Article  Google Scholar 

  • Talbot MR, Livingstone DA (1989) Hydrogen index and carbon isotopes of lacustrine organic matter as lake level indicators. Palaeogeogr Palaeoclimatol Palaeoecol 70:121–137

    Article  Google Scholar 

Download references

Acknowledgments

We thank T. C. Moore for his helpful comments on our statistical analyses. This study was supported by the “PALEOTRACES” International Mixed Laboratory between Institut de Recherche pour le développement, Universidade Federal Fluminense and Universidad de Antofagasta, as well as by the CLIMPAST project (CNPq-IRD), which corresponds to the international cooperation project between the Brazilian CNPq and the IRD (Processo CNPq n°: 490735/2006-1). The authors sincerely thank the ESCARSEL ANR for financial support. Finally, we deeply appreciate the constructive comments from the reviewers and editors that helped us to improve this contribution.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Philip A. Meyers.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Sifeddine, A., Meyers, P.A., Cordeiro, R.C. et al. Delivery and deposition of organic matter in surface sediments of Lagoa do Caçó (Brazil). J Paleolimnol 45, 385–396 (2011). https://doi.org/10.1007/s10933-011-9506-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10933-011-9506-0

Keywords

Navigation