a b s t r a c tSixteen Argentinean shallow lakes from the Pampa plains and the Patagonian steppe were characterized using optical properties and water-quality parameters. In this set of lakes a wide range in water transparency descriptors was observed [broadband vertical attenuation coefficient (kd PAR) varied from 0.40 to 47 m À1 , Secchi disk depth (Sd) from 0.07 to 12.00 m, and nephelometric turbidity (t n ) from 0.50 to 103.70 NTU (710.00)]. Among Pampean lakes, highly turbid lakes presented significant higher kd PAR values (413 m À1 ) than clear-vegetated ones (o10 m À1 ), though all Patagonian lakes showed significant lower light attenuation (kd PARo2.5 m À1 ). Our estimations of light scattering were supported by the significant relationship found between t n and Effler and Auer's scattering coefficient estimate (b est ). Allowing for lakes with t n o80 NTU, we obtained a significant linear regression with a slope close to the unity. However, when values of t n were higher than 80 NTU, no clear relationship was observed between t n and b est .Although we found significant relationships between kd, Sd and t n over the whole range of underwater light scenarios, we noticed some disparities between Sd, t n and light attenuation in lakes with certain optical characteristics. Considering the whole data set, including clear and turbid lakes, as much as 92% of the variation observed in kd PAR could be explained by a regression model including absorption of chromophoric dissolved organic matter (CDOM) and t n .Our results showed that a suitable and practical method to estimate light attenuation could be the use of empirical models based on absorption coefficients and t n measured with bench top instruments. The direct measurement of paired values of Sd and t n , in addition with main absorbing components are a useful and precise way of describing underwater light availability and optical regimes. The latter, combined with occasional in situ measurements of kd would permit the development of highly accurate lake-specific models of light attenuation.