Macrophytobenthos biomass in the Northwestern Cuban shelf, almost 50 years ago
Graphical abstract
The percent frequency to percent biomass ratio was 2.28 for sea weeds, and 0.55 for seagrasses. For brown and red seaweeds combined was 1.43 or 39 % smaller than the 2.33 for green seaweeds because of the calcium carbonate contents of five Halimeda, two Penicillus, Rhipocephalus phoenix, and two Udotea species. Consequently those Rhizophytic algae, with 72 % of the total frequency, represented 76 % of the total wet biomass of all green seaweeds during this 1972−1973 baseline research. The result was that seagrasses had the most biomass, while the seaweeds the greater frequency.
Introduction
Cuba, the largest of the Greater Antilles, is an archipelago composed of a main island and approximately 1600 additional islets and cays (Knight and Levinson, 2019) with four unequal shelves, two wider and larger in the South, and two narrower and smaller in the North separated by depths in excess of 1000 m.
In 1964 artisanal fisheries in Cuban national waters took place in these four platforms. Total landings were 23,400 tons, 96 % corresponding to demersal species caught between the coast and the 200 m isobath, of which almost 26 % were caught in the Northwestern shelf (Buesa, 1964).
From San Antonio cape to La Mulata port the NW shelf can be divided into two areas: the larger, wider, and deeper Gulf of Guanahacabibes (GG) to the West, and the smaller, narrower and shallower Buenavista Cays to La Mulata port (BLM) 258 km to the East. From La Mulata port to Matanzas bay, 200 km further east, there is no a real submersion shelf, the 200 m isobath is seldom 100 m off the coast, and is the site of a minor marlin and swordfish pelagic fishery.
The phytoplankton primary production from surface to 25 m depth in the GG area was 0.36 gC.m−2.d-1 in 1964 (Kondratieva and Sosa, 1967) and it was 0.30 gC. m-3.d-1 in 1965 (Kabanova and López-Valuja, 1973). In 1964, the zooplankton fresh biomass was 0.4 to 1.5 g.m−2 from surface to 10 m depth (Marikova and Campos, 1967), sustaining a minor clupeid fishery (Silva, 1974).
In 1963, the total combined commercial catch of both areas of this platform was 2.24 g.m−2, of which 28 % were spiny lobsters, and 58 % benthophagous fish species (Buesa, 1964). In 1964 the zoobenthos biomass was 45.3 g.m−2 with greater abundance and fresh biomass (69.1 g.m−2) in turtle grass meadows, than on silty sand bottoms (Murina et al., 1969). By 1986–1990 the total annual average commercial catch had been reduced 59 % to 0.92 g.m-2 of which 8% were spiny lobsters, and 74 % corresponded to 32 finfishes (Claro et al., 2001; González-Sansón and Aguilar-Betancourt, 2007).
The high productivity of the platform is also noticeable in the primary production of its phytobenthos, with turtle grass (Thalassia testudinum) producing 4.7 gC. m−2.d-1 in a coastal meadow off Playa Habana in 1971 (Buesa, 1972). Assuming that P/B was constant throughout the shelf, and with knowledge on biomass distribution of the species across the shelf, Buesa (1974) estimated a production of 5.2 gC. m−2.d-1, almost 16 times that shelf’s average phytoplankton primary production. Impressive as such primary production difference was, it is a minimal estimate of phytobenthos production, as many more macrophytobenthos species are found on the shelf.
The objective of this manuscript is recording the biomass of all macrophytobenthos species on the NW Cuban shelf during a 1972−1973 sampling campaign. These data, can also serve as a comparison baseline with present and future data, especially for turtle grass meadows because, seagrasses are declining globally (Waycott et al. (2009), and historical data on larger meadows extensions providing baseline data measuring possible changes on biomass and cover of seagrass meadows are scarce, but essential to assess the present state of these vulnerable ecosystems.
Section snippets
The Northwester submersion shelf characteristics
The sampling area was from San Antonio cape (21.87 °N/84.95 °W), the western most tip of Cuba to La Mulata port (23.13 °N/82.38 °W) 258 km to the East. It is a proper submersion platform that can be divided in two areas: the Gulf of Guanahacabibes (GG), roughly triangular in shape, extends from San Antonio cape to the West, to La Fe port (22.03 °N/84.41 W) to the East, and to Buenavista cays (22.40 °N/ 84.41 °W) to the North. The other area is from Buenavista cays to La Mulata port
Environment
During the four trips the average subsurface (at 0.5 m depth) water temperature was 28.4 °C (24.0 °C–31.0 °C range, N = 213 stations), and average at bottom (at 7.9 m depth) was 28.0 °C (23.5 °C–35.5 °C range, N = 156 stations), indicating a well-mixed water column. Depending on depth, the percentage of surface light reaching the bottom was from 4% to 87 % (49 % average at 7.9 m depth) assuring 1.4 kW.m−2.s-1 solar bottom irradiation at noon. More details on the oceanographic data can be found
Discussion and conclusions
At present, many intentions of mapping the seagrasses are being made (Wabnitz et al., 2008) to understand the extension of the seagrass meadows, and the abundance of their components is becoming of more vital importance, considering the gradual changes and losses of these meadow suffer from increasing anthropogenic pressures (Waycott et al., 2009). However, early data on seagrass and algal distribution are scarce, and this work on the macrophytobenthos distribution in the Northwestern Cuban
Declaration of Competing Interest
The authors report no declarations of interest.
Acknowledgements
After the 1972 summer trip the author sent to Cornelius den Hartog, presently Professor Emeritus at the University of Nijmegen, several Halodule wrightii and Halophila decipiens specimens for identification confirmation, which he did. Margaret Greenway, presently Adjunct Professor at the School of Engineering and Built Environment, Griffith University, Brisbane, Australia commented the initial draft of this report. My sincere appreciation to both and five anonymous reviewers of this manuscript
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