Luquillo Data Sets By Insertion Order
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Numeric Dataset ID |
Data Set Identifier | Abstract | Owner | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| 24 | Anoline Lizard Food Habits |
The stomach contents of 10 adult individuals of each of three anole species (Anolis gundlachi, A. evermanni, and A. stratulus) were collected to determine the number, type, and volume of prey consumed following Hurricane Hugo. Gut contents were identified to the lowest taxon possible and were measured. |
Douglas Reagan | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 23 | Bird abundance - point counts |
Circular plot counts are used to measure relative numbers of birds over time and between sites. The duration of each count is 10 minutes. During this period, all birds heard or seen are recorded on a data sheet in one of two categories: 1) within 25 m of the observer (< 25 m) and 2) further than 25m from the observer (> 25 m). Records are further broken down into birds only heard (H on the data sheet) and birds observed (recorded as estimated distance from the sampling point in meters; see sample data sheet). Counts are begun as soon after dawn as possible and conclude before noon. Census points are at least 60 m apart within the grids. A complete list of the grid points where counts are taken is found in the data. Originally counts were conducted three times a year. |
Robert B. Waide | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 22 | Cecropia growth at El Verde gaps |
While doing the survey of gaps at El Verde the number and height of Cecropia saplings found in gaps where recorded. Since this species is mostly restricted to gaps, an estimate of the total population of Cecropia in the regeneration size classes in the forest can be obtained. (There are others along the edges of the Sonadora and Prieta.) The abundance, dispersion, and size class distribution of the Cecropia population is an index of disturbance in tabonuco forest and make an interesting study in its own right. |
Nicholas Brokaw | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 21 | Vegetation profile and canopy height of Tabonuco, Colorado and Cloud Forests |
The overall height and the presence of vegetation in different height intervals above ground is recorded above points on a 5 x 5 m grid in three hectare-sized plots in the Luquillo Experimental Forest, Puerto Rico. One plots each is in tabonuco forest (350 m elevation), colorado forest (650 m) and cloud forest (1000 m). The first records were made shortly before Hurricane Hugo, in 1989. Post hurricane measurements have been made five time to six time in each plot, the most recent been in 1998 for all plots. The results show the damage to forest structure wreaked by Hurricane Hugo, steady recovery of forest structure after Hugo, minor damage by Hurricane Hortense in 1996, and resumption of recovery after Hortense. Maximum canopy height and the vertical distribution of vegetation in the forests are returning to pre-hurricane Hugo values. |
Nicholas Brokaw | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 20 | Chemistry of stream water from the Luquillo Mountains |
Stream water is collected weekly at the Luquillo Mountain sites listed below. These data sets begin as early as 1983; LTER sampling began in 1988. Stream water samples are grab samples taken from the water/air interface at stream channel center on the sampling day (usually Tuesdays). A continuous record of stream stage (height) is recorded by a datalogger at all ongoing stream sampling sites. Average daily streamflows are available from the USGS and at other locations (Hydrology and Meteorology) on this site. All samples are measured for pH and conductivity, and then filtered (pre-combusted Whatman GF/F glass fiber filter) prior to further analysis. From 1983-1994 samples were cooled and returned to the San Juan chemistry laboratory for analysis. During those years, samples for NH4 and NO3 analyses were refrigerated continuously until analysis. Subsamples for NH4 analysis were also preserved with 1 molar H2SO4. From 1994 on, samples for NH4 and NO3were frozen until analysis, were not acidified, and all analyses were conducted at the University of New Hampshire.
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William H. McDowell | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 18 | Revegetation of landslides, vegetation > 1.0m (Large landslide plots at the Luquillo Experimental Forest) |
Here we use permanent plot data sampled from 16 landslide to documents temporal successional pathways in landslide patches (without the use of a chronosequence, cf. Guariguata 1990) and address the following questions: (1) What are the successional pathways of landslide and what species define them? How much pathway variation of individual plots is there within these landslides? (2) How similar are pathways among landslide? Is there any evidence that, with time, landslides either converge to a common vegetative enpoint or slow in the rate of successional change? The purpose of this study is to document the recovery of vegetation on new landslides in the Luquillo Experimental Forest. |
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| 17 | Minimum temperature at El Verde Field Station, Rio Grande, Puerto Rico since 1975 |
Daily emperature has been measured at the El Verde Field Station since 1975 (see methods). Monthly averages have been calculated. Lowest average values for minimum temperature were recorded from January to April with nearly 18 Centigrades during this period of time (see chart). During these months, the lowest average minimum temperature was recorded in 1976 ranging from 20 to 22 Centigrades (see chart). Highest minimum montly average records are shown from June to October with peak in the vecinity of 20 Centigrades. The year with lowest minimum tempearture was 1995 and 2000 with the low values near 14 and 15 Centigrades, respectively. |
Alonso Ramirez | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 16 | Maximum temperature at El Verde Field Station, Rio Grande, Puerto Rico since 1975 |
Daily emperature has been measured at the El Verde Field Station since 1975 (see methods). Monthly averages have been calculated. Maximum values for maximum temperature were recorded from May to October with a range from 29 to 30 and peaks of 29.7 Centigrade in October. The months of October through December show the most dramatic increase, specially December (see chart). Highest average maximum temperatures during these years were recorded in 1998 and 1999 (See chart). Max monthly temperatures appear to be increasing from this years on. |
Alonso Ramirez | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 15 | Revegetation of landslides, vegetation <0.1m (Small landslide plots at the Luquillo Experimental Forest) |
The purpose of this study is to document the recovery of vegetation on new landslides in the Luquillo Experimental Forest, in particular seedlings <1m tall. |
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| 14 | Rainfall at El Verde Field Station, Rio Grande, Puerto Rico since 1975 |
Rainfall has been measured at the El Verde Field Station since 1964. McDowell and Estrada-Pinto, 1988 presents a description of the collection procedures, raw data from 1964 to 1986, and some summary statistics for this period of record. Precipitation for this period showed some seasonality in monthly means, with a peak in May. Monthly averages for the period of 1975 to current chart can be found at this site. The highest values for the monthly averages for the period of 1975 to 2000 are from August to December with a low in October and November the highest. In this period the highest amount of total annual rainfall was in 1998 with 5293.61 mm and the minimum in 1994 with 1402.87 mm. |
Alonso Ramirez | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 8 | Canopy gap survey at El Verde |
The survey of gaps at El Verde covers about 35 ha, including the 9 ha grid. We defined a treefall gap at El Verde as a hole in the forest canopy extending down to an average height of about 3 m or less above ground. The edge of a gap was delineated by the vertical projection of the edge of the canopy foliage. We measured the dimensions of all gaps present in the 35-ha study site in August 1989, one month before Hurricane Hugo. For each gap we measured L, the longest axis of the gap (distance between edges), and W, the longest axis perpendicular to L, and then approximated gap area as that of an ellipse: Area = p LW/4 (Runkle 1992). Only openings ³ 20 m2; were counted as gaps. |
Nicholas Brokaw | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 7 | Soil sample from landslide ES1 (Espiritu Santo El Verde), ES2, and RB2 (Rio Blanco) |
Analysis of soil nutrients in top 9 cm of soil in Landslide Revegetation Plots. |
Lawrence R. Walker | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 6 | Anole grid study (El Verde 9Ha and Bisley) |
Transects 60 m long are conducted at alternate points in the 9 ha grid at El Verde. Transects 80 m long are conducted at alternate points at the Bisley Grid in watersheds #1 and #2. Data are used to support the GIS database. |
Douglas Reagan | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 5 | Anole Mark and Resight Study |
The population distribution research area of the LEF LTER is designed to gather information on the distribution and abundance of key plant and animal species within the forest under different disturbance regimes. Multiple mark and resight studies were conducted to determine the population density of Anolis stratulus at one undisturbed forest site and one site in a partially regenerated treefall gap. Tower surveys were conducted in order to access individuals in the forest canopy. |
Douglas Reagan | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 4 | Anole Vertical Transects (tower data) |
Transects are conducted to note the vertical distribution and relative abundance of anole species. Data permit the calculation of average sighting distance for each species which is used in the final calculation of abundance. |
Douglas Reagan | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 2 | Anole treefall gap transects (Bisley and El Verde-H10 Gaps) |
Transects were established through large recent treefall gaps to determine the relative abundance of different anole species at different distances from the center of the gap. |
Douglas Reagan | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 1 | Anole ground level transects (Bisley and El Verde) |
Transects are surveyed through the upper and lower cut plots at Bisley to determine the distribution and minimum abundance of anoles within and adjacent to the plots. Surveys began prior to cutting will continue seasonally (wet and dry) to document changes as the plots regenerate. One set of two transects has been established near the walkway towers in the 9 ha grid at El Verde. Each transect is 90 m long (wet 1989 and dry 1990) and 120 m long thereafter. Two transects, each 120 m long are established near the tower at Bisley. Survey methods and data recorded are the same for all transects, except that distance along the transect is recorded for cut plot transects only. |
Douglas Reagan |