Frustules are cylindrical, join face-to-face and form filamentous colonies. Valves are 4-17 µm in diameter, with a mantle height of 4-20 µm. The ratio of the mantle height to valve diameter is usually greater than 0.8 but less than 5. The mantle has straight sides and the valve face is flat. The mantle areolae are square. The rows of areolae on the mantle are curved to the right (dextrorse), but often are almost straight and parallel to pervalvar axis in separation valves and number 8-18 in 10 µm. The valve face has small scattered areolae more densely distributed around the valve face margin. Linking spines are located at the end of each pervalvar costa. Linking spines are short, triangular or bifurcated. Separation spines originate from two pervalvar costae. Most separation spines are 2-6 µm long, but a few, usually 1-2 spines per valve, are very long, almost equal in length to the valve mantle. The ringleiste is solid and moderately shallow. Coiled rimoportulae are usually positioned along a stria on the mantle at the distance of 1-3 areolae from the collum and and similarly along a stria, but much closer to the valve face.
Density and arrangement of the mantle areolae varies considerably among populations and even among cells within a single colony depending on environmental conditions (Stoermer et al. 1981). For the populations found in the Great Lakes the following informal classification of morphotypes was proposed by Stoermer et al. (1981): status α specimens have coarse areolae (8-12 rows in 10 µm, 8-12 areolae in 10 µm in a row) and usually straight rows in separation valves, but spiral in linking valves; status γ specimens have fine areolae (13-18 rows in 10 µm, 13-18 areolae in 10 µm in a row) have only spiral rows of areolae; status β specimens have both types of valves within a colony.
Populations with long thin cells approximately 3-4 µm in diameter have been described as A. granulata var. angustissima (Otto Müller) Simonsen, but Kilham & Kilham (1975) showed that this, as well as another variety A. granulata var. ionensis (Grunow) Simonsen represent morphological variations within the life cycle of A. granulata. We observed a break in the distribution of valve diameters and mantle height/valve diameter ratios in natural populations of A. granulata sensu lato from the US, and for that reason recommend separating the variety angustata from the nominate variety until additional studies clarify the taxonomy of this species complex. No break is observed, however, in the distribution of valve diameters and mantle height/valve diameter ratios between A. granulata and A. muzzanensis, and all other characters appear to overlap between two species. Until further studies clarify the taxonomy of this species complex, we recommend differentiating these two species using this decision rule: if the ratio of the mantle height to valve diameter in at least some cells in a colony is less than 0.8, or if it is between 0.8 and 1.2 and areolae are coarse and disorganized, a specimen is identified as A. muzzanensis. If this ratio in all cells is greater than 0.8, or it is between 0.8 and 1.2, but areolae are organized in regular rows, it is identified as A. granulata.
Colonies are usually straight, but sometimes spiral, with curved cells. Such populations have been described as separate forms of A. granulata (A. granulata f. curvata (Hustedt) Simonsen) and A. granulata f. spiralis (Hustedt) Czarnecki & Reinke, but there is no evidence that this trait has taxonomic significance.
This taxon is reported to be widespread in freshwater (Foged 1977, Foged 1981, Cox 1996), however, phylogenetic analyses suggest that this taxon may be a species complex (Edgar and Theriot 2004, Van de Vyver et al. 2022). Verified reports from North America are from Alaska (Foged 1981), Utah (Grimes and Rushforth 1982, Bateman and Rushforth 1984), and British Columbia (Cumming et al. 1995), the St Lawrence River (Reavie and Smol 1998), the Great Lakes (Reavie and Kireta 2015), North Carolina (Bishop et al. 2017), Texas, Arkansas (SMM MBE - 2610 pers. obs. LA, 2019) the Rocky Mountains, Great Plains, California Central Valley, Puget Trough, and Willamette Basin (Bahls 2021). Bahls (2021) noted that this taxon was largely absent from the Cascades. Bahls (2021) reports this taxon to occur primarily in lakes, reservoirs and rivers with dams, but also in smaller rivers and streams. Barinova et al. (2023) report this taxon from planktonic and benthic habitats.
In the Great Lakes National Parks (Edlund et al. 2011, 2012, 2013), it is common (1-10% relative abundance) in sediment core material from lakes in Isle Royale (Richie and Ahmik lakes) and St. Croix National Scenic Riverway (Lake St. Croix), (Edlund et al. 2009).
This taxon is reported to prefer alkaline waters (Foged 1981, Bahls 2021, Barinova et al. 2023) with moderate (Bahls 2021) to high (Cox 1996, Bartozek et al. 2019, Wengrat et al. 2019, Barinova et al. 2023) nutrient content. Barinova et al. (2023) report this taxon to be saprophilic.
Many authors recognized forms we are currently treating as A. granulata var. angustisssima on diatoms.org within the morphological concept of the nominate variety (e.g, Clark and Rushforth 1977).
Many research groups consider this taxon an indicator organism and published regional environmental optima and tolerances including:
Sovereign (1958): pH 5.5-9.0 for populations observed from Upper Klamath Lake and Diamond Lake.
Fallu et al. (2000): Dissolved Organic Carbon – 13.16 +/- 1.30 mg/L for populations from Quebec.
Reavie and Smol (2001): Total Phosphorus (TP) – 0.019 mg/L, pH – 8.20, Total Nitrgen (TN) – 0.508 mg/L, Max Depth – 14.4 m, Chla – 1.81 mg/L from populations in southeastern Ontario.
Reavie and Kireta (2015): Report TP optima to be well above 30 µg/L, and Cl optima to be between 10 and 50 µg/L for populations from the Great Lakes.
Bicudo et al. (2016): Temperature – 19.53 °C, pH – 6.82, Conductivity – 139.32 µS/cm, Alkalinity – 0.55 mE/L, P-PO4 – 25.85 µg/L, Dissolved Inorganic Nitrogen – 845.1 µg/L, TP – 55.81 µg/L, TN – 1518.14 µg/L for populations from tropical reservoirs in Brazil.
Bahls (2021): Abundance Weighted Mean (AWM) pH – 8.1, AWM Conductivity – 639 µS/cm, AWM Temperature – 17.2 °C, AWM Total Nitrogen – 770 µg/L, AWM Total Phosphorus – 61 µg/L for populations from the western US.
Barinova et al. (2023): pH – 5.8-9.4
From 2010 until 2024 the autecological information on this taxon page was limited. As of this update, information on ecology, biogeography, and environmental optima have been added. - Lane Allen & Mark Edlund
Potapova, M., English, J., Allen, L., Edlund, M. (2010). Aulacoseira granulata. In Diatoms of North America. Retrieved November 23, 2024, from https://diatoms.org/species/aulacoseira_granulata
The 15 response plots show an environmental variable (x axis) against the relative abundance (y axis) of Aulacoseira granulata from all the stream reaches where it was present. Note that the relative abundance scale is the same on each plot. Explanation of each environmental variable and units are as follows:
ELEVATION = stream reach elevation (meters)
STRAHLER = distribution plot of the Strahler Stream Order
SLOPE = stream reach gradient (degrees)
W1_HALL = an index that is a measure of streamside (riparian) human activity that ranges from 0 - 10, with a value of 0 indicating of minimal disturbance to a value of 10 indicating severe disturbance.
PHSTVL = pH measured in a sealed syringe sample (pH units)
log_COND = log concentration of specific conductivity (µS/cm)
log_PTL = log concentration of total phosphorus (µg/L)
log_NO3 = log concentration of nitrate (µeq/L)
log_DOC = log concentration of dissolved organic carbon (mg/L)
log_SIO2 = log concentration of silicon (mg/L)
log_NA = log concentration of sodium (µeq/L)
log_HCO3 = log concentration of the bicarbonate ion (µeq/L)
EMBED = percent of the stream substrate that is embedded by sand and fine sediment
log_TURBIDITY = log of turbidity, a measure of cloudiness of water, in nephelometric turbidity units (NTU).
DISTOT = an index of total human disturbance in the watershed that ranges from 1 - 100, with a value of 0 indicating of minimal disturbance to a value of 100 indicating severe disturbance.