Corals and coral reefs of the Puerto Angel region , west coast of México

Resumen: Se presentan datos sobre la riqueza de especies y las características de tres arrecifes de coral de la región de Puerto Angel, México (15° N), visitados en 1994 y revisados en seis censos visuales de una hora, conducidos hasta 6 m de profundidad. Se encontró un total de siete especies en el área (pertenecientes a cuatro géneros), siendo la más abun­ dante PociUopora damicomis (L., 1758). Las especies de este género fueron las principales constructoras de la estruc­ tura arrecifal en los sitios visitados. Los corales masivos fueron poco comunes, y habitaban principalmente en la base de los arrecifes. Por la presencia de una estructura arrecifal bien cementada y una zonación clara, los arrecifes de fran­ ja de Puerto Angel deben ser considerados entre los mejor desarrollados de la costa del Pacífico de México. Un evento de mortalidad coralina y posterior recolonización fue observado en esta visita. Sin embargo, no se determinó cuál fue su causa.

The coral communities and reefs of the east ern tropical Pacific have been studied for more than a hundred years (Guzmán & Cortés 1993).However, data are still lacking from several long coastal margins, especially in México, where coral communities and reefs are well known only in the Gulf of California (Squires 1959, Reyes-Bonilla 1993).
The objective of this paper is to describe the general composition and structure of three coral reefs located near Puerto Angel, México: Playa Panteones, Playa Ixtacahuite and La Guacha (Fig. 1).Palmer (1928) reviewed the geologic history of this area, described three species, and point out sorne general characteristics of local reefs.Later, the presence of two other coral species was confirmed (Geister 1975, Rodríguez Palacios et al: 1988) and recently, Glynn & Ley te-Morales (1997) and Ley te-Morales (1997) mentioned all reef areas located north of the Gulf of Tehuantepec, presented an updated species list, and emphasized the need for con servatíon of this biological systems.
The coral communities of Puerto Angel area occupied a small plateau that gradually reached 15 to 20 m depth at a dístance of 50 to 100 from shore.The site is located near the Isthrnus of Tehuantepec and local upwellings may occa sionally affect the coral communities (Lluch Cota et al. 1997).Average sea surface temper ature outside of Puerto Angel bay is 280C ± 1.8 (Anonymous 1982(Anonymous -1995)).Salinity fluctuates from 33.5 to 34.5 ppm, and thermocline depth is stable at 60 m almost all year round in the area where coral development occurs (Fiedler 1992).
For this study, a total of six one-hour visual surveys were conduced at the three localities during January 1994, with snorkel and SCUBA equipment and at depths from O to 6 m.Specimens of all the coral species observed were collected and deposited at the Instituto de Recursos, U. del Mar.Taxonomic determina tions followed Wells (1983) and Veron (1986) criteria.Seven species were found in the area: Pocillopora damicornis (L., 1758), P. capitata Verrill, 1864, P. meandrina (Dana, 1846), P. ver rucosa (Ellis & Solander, 1786), Pocillopora sp., Pavona gigantea Verrill, 1869 and Porites pana mensis Verrill, 1866.Of these, Pocillopora dam icornis was consistently the most abundant species in aH the localities, followed by P. capi tata; both were distributed mainly from 1 to 10m depth, decreasing their abundance with depth.Other pocilloporid species were uncornmon.Colonies of Porites panamensis were extremely scarce, encrusting, and appeared only at depths < 3 m.The agaricid Pavona gigantea was rare at all reefs, but it developed large colonies (> 1 m height), especially on rocky zones and at depths from 3 to 5 m.

OCÉANO PAciFICO
The presence of an undescribed species (Pocillopora sp.) was one of the most remark-able findings.Its most distinctive character is that, unlike all other pocilloporids of the east Pacific, this one had no branches, but instead developed colonies with completely fiat upper surfaces.The coralla are composed by pave ments of polyps arranged in several levels, each one of these physically separated from the next.AH levels are built by consecutive series of polyps (Ley te-Morales in prep.).
At La Guacha and Ixtacahuite, the reef framework projected 1 to 3 m from the bottom, it was well consolidated and composed predom inantly of cemented pocilloporid corals.Large portions of its uppermost section and sides were dead and covered with coralline and fieshy algae and barnacJes, but also had numerous small pocilloporid colonies (15 to 20 cm maxi mum diameter, 3 to 5 cm height) scattered over.Those coralla were classified as recruits, since a discontinuity among the framework and the base of the new coral existed (they were not fragments).AIso, colonies were almost sym metrical and stemmed from one point, an indi cation of larval origin (Richmond 1987).Massive coral s were almost absent in the main framework area, but they became increasingly common in the base of the reef (> 5 m depth).
Befare the visit, we supposed that the reefs of the Puerto Angel area may have a large num ber of species because of their cJoseness to the main eastern Pacific reefs at Central America, and of a possible larval transport from the north.The actual number of recorded species (seven) is, however, very low.During field work we did not find several taxa which have been already seen in nearby sites, like Gardineroseris planu lata (Dana, 1846) or Pavona varians Verrill, 1864 (Ley te-Morales 1997).The presence of sandy bottoms at north and south of Puerto Angel and the upwellings in the Gulf of Tehuantepec may be acting as isolating forces, limiting larval arrivaJ, and restricting the num ber of coral species (Glynn & Ley te-Morales 1997).
The good development and zonation of the Puerto Angel reefs should result of the adequate local thermal conditions (mean monthly tem perature is never lower than 270 C in the year; Fiedler 1992).These well-structured communi ties are potentially as old as others that show similar conditions elsewhere (Guzmán & Cortés 1993).In comparison, zonation and large frameworks are uncommon at the apparently younger coral areas of the Gulf of California and the Revillagigedos (Squires 1959, Reyes Bonilla 1993).
1ñere ar e no reports of effects-that -El-Niño events may have had on reef coral s of Puerto Angel, although small thermal anomalies occurred in 1983 «1.50 C; Lluch-Cota et al. 1997).Notwithstanding, large tracts of dead coral covered by algae were seen in 1994, all of them invaded and eroded by sea urchins (Diadema Gray, 1825, Echinometra Gray, 1825, Eucidaris Mortensen, 1909, Centrostephanus Peters, 1855 and Toxopneustes Agassiz, 1841), as it occurred at several bleached sites after 1982-83 (Guzmán & Cortés 1993).If the coral mortality of Puerto Angel was not a con se quence of an ENSO, it may have been a human caused event; human population has increased considerably in the coast in the last decade because of the creation of a large government owned touristic infrastructure, which may have affected the coral communities in sorne way.However, we have no data to point to any factor as the actual cause of the dead coral tracts.New studies• on this coral reefs will help to answer our questions and to evaluate its importance.
The visit of H.R.B. to Puerto Angel was sup ported by Juan Gabriel Díaz U. and Silvia Ramírez L. (UMar).Jose Carriquiry (110-UABC, Ensenada) reviewed the manuscript and commented on several aspects here discussed.Two anonymous reviewers also suggested important additions for the papero