What's the temperature in tropical caves?

Hourly temperature was measured for approximately one year at 17 stations in three caves in Quintana Roo, Mexico. Thirteen of these stations were in the extensive twilight zones of all three caves. All seventeen stations showed seasonality in temperature with a 3°C drop during the Nortes season. Two of the caves, Muévelo Sabrosito and Muévelo Rico, showed greater variability during the winter months while in Río Secreto (Tuch) variability was greatest during the rainy season. Río Secreto is less open to the surface than the other two. All sites also showed a daily temperature cycle, although it was very faint in some Río Secreto (Tuch) sites. While temperature variability is diminished relative to surface variation, its temporal pattern is worthy of further study.

Nutrient availability in tropical caves influences the dynamics of microbial biomass.

Few studies have evaluated the trophic level in tropical caves, and none related the microbial biomass dynamics in the immobilization of carbon and nitrogen. Here, four tropical caves of Terra Ronca State Park, Brazil, were studied: Angélica, São Bernardo, Terra Ronca I, and Terra Ronca II caves. Physical, chemical, and microbiological parameters (microbial biomass and respiration) were estimated in the dry and wet seasons. São Bernardo, Terra Ronca I, and Terra Ronca II caves presented higher nitrogen and microbial biomass nitrogen (MBN) values in the wet season than in the dry season. On the other hand, the Angélica cave showed larger amounts of nitrogen and lower MBN values in the dry season. These results indicate that caves can be adjusted in two ecological theories known as "stoichiometric decomposition" and "microbial nitrogen mining"-to the effects of nutrient availability on organic matter decomposition. The caves studied showed different environmental dynamics in relation to organic matter decomposition, which allows them to be considered unique and possess specific characteristics. Microbial biomass dynamics can be an important parameter to evaluate the availability of nutrients and ecological dynamics of the trophic network in subterranean environments.

Radon (222Rn) concentrations in the touristic Jumandy cave in the Amazon region of Ecuador.

This work consists of the detection and quantification of the concentration levels of radioactive gas radon-222 (222Rn) of natural origin, as well as the determination of the critical points and the estimation of the effective dose absorbed by the tourists and guides inside the Jumandy cavern in Napo, Ecuador. According to the feasibility map of uranium of Ecuador, the study area is located in one of the top-priority areas for obtaining uranium, suggesting possible radioactivity in this unstudied region. The measurements were carried out from July to October of 2017, in three different monitoring points inside the cavern. The average radon concentrations measured in the cavern exceeded the maximum recommended environmental level by a factor of 28, and the effective dose absorbed by the guides exceeded the recommended maximum by a f actor of 10. Meteorological parameters such as temperature and relative humidity have an impact on the 222Rn concentrations in different parts of the cave.

Population density and habitat of an endangered cave fish Eigenmannia vicentespelaea Triques, 1996 (Ostariophysi: Gymnotiformes) from a karst area in central Brazil

The troglobitic electric fish Eigenmannia vicentespelaea, endemic to a single cave-system and included in the Brazilian Red List of Threatened Fauna, was studied in relation to population densities and habitat. For comparison, we used the epigean species, E. trilineata. We verify if the population densities recorded for E. vicentespelaea follow the pattern observed for other subterranean fishes; if there are seasonal fluctuations in these densities and which environmental variables explain the densities variation. We estimated abundances and population densities during three consecutive dry seasons concomitant with habitat description and physicochemical variables measurements. For E. vicentespelaea: in six stream reaches in the São Vicente II cave. For E. trilineata: from counts of active fish in rio da Lapa. The mean population density recorded for E. vicentespelaea is considered low (0.17 ind.m-2), similar to those of E. trilineata (0.13 ind.m-2), without significant differences between the years, but with marked fluctuations during dry seasons within each year, suggesting seasonality. Estimated population size of E. vicentespelaea is considered low (270 individuals in average). Depth, water current and substrate, allied to plant debris explain better the variation of densities. Urgent actions for E. vicentespelaea conservation include protection of headsprings in Terra Ronca State Park.(AU)

O peixe troglóbio Eigenmannia vicentespelaea, endêmico de um único sistema de cavernas e incluído na Lista Brasileira de Fauna Ameaçada foi estudado em relação às densidades populacionais e hábitat. Para comparação utilizamos a espécie epígea E. trilineata. Verificamos se as densidades populacionais registradas para E. vicentespelaea seguem o padrão observado para outros peixes subterrâneos; se há flutuações sazonais nestas densidades e quais variáveis ambientais explicam as variações nas densidades. Estimamos as abundâncias e densidades populacionais ao longo de três estações secas consecutivas, concomitantes à descrição do habitat e das variáveis físico-químicas. Para E. vicentespelaea: em seis trechos de rio ao longo da caverna São Vicente II. Para E. trilineata: na contagem de peixes ativos no rio da Lapa. A densidade populcional média registrada para E. vicentespelaea é baixa (0,17 ind.m-2), similar à observada para E. trilineata (0,13 ind.m-2), sem diferenças significativas entre os anos, mas com flutuações marcantes ao longo das estações secas dentro de cada ano, sugerindo sazonalidade. O tamanho populacional estimado para E. vicentespelaea é considerado pequeno (270 indivíduos em média). Profundidade, correnteza, substrato, aliadas à concentração de detrito vegetal explicam melhor a variação nas densidades. Ações urgentes para conservação de E. vicentespelaea incluem a proteção das nascentes do Parque Estadual de Terra Ronca.(AU)

Population density and habitat of an endangered cave fish Eigenmannia vicentespelaea Triques, 1996 (Ostariophysi: Gymnotiformes) from a karst area in central Brazil

The troglobitic electric fish Eigenmannia vicentespelaea, endemic to a single cave-system and included in the Brazilian Red List of Threatened Fauna, was studied in relation to population densities and habitat. For comparison, we used the epigean species, E. trilineata. We verify if the population densities recorded for E. vicentespelaea follow the pattern observed for other subterranean fishes; if there are seasonal fluctuations in these densities and which environmental variables explain the densities variation. We estimated abundances and population densities during three consecutive dry seasons concomitant with habitat description and physicochemical variables measurements. For E. vicentespelaea: in six stream reaches in the São Vicente II cave. For E. trilineata: from counts of active fish in rio da Lapa. The mean population density recorded for E. vicentespelaea is considered low (0.17 ind.m-2), similar to those of E. trilineata (0.13 ind.m-2), without significant differences between the years, but with marked fluctuations during dry seasons within each year, suggesting seasonality. Estimated population size of E. vicentespelaea is considered low (270 individuals in average). Depth, water current and substrate, allied to plant debris explain better the variation of densities. Urgent actions for E. vicentespelaea conservation include protection of headsprings in Terra Ronca State Park.

O peixe troglóbio Eigenmannia vicentespelaea, endêmico de um único sistema de cavernas e incluído na Lista Brasileira de Fauna Ameaçada foi estudado em relação às densidades populacionais e hábitat. Para comparação utilizamos a espécie epígea E. trilineata. Verificamos se as densidades populacionais registradas para E. vicentespelaea seguem o padrão observado para outros peixes subterrâneos; se há flutuações sazonais nestas densidades e quais variáveis ambientais explicam as variações nas densidades. Estimamos as abundâncias e densidades populacionais ao longo de três estações secas consecutivas, concomitantes à descrição do habitat e das variáveis físico-químicas. Para E. vicentespelaea: em seis trechos de rio ao longo da caverna São Vicente II. Para E. trilineata: na contagem de peixes ativos no rio da Lapa. A densidade populcional média registrada para E. vicentespelaea é baixa (0,17 ind.m-2), similar à observada para E. trilineata (0,13 ind.m-2), sem diferenças significativas entre os anos, mas com flutuações marcantes ao longo das estações secas dentro de cada ano, sugerindo sazonalidade. O tamanho populacional estimado para E. vicentespelaea é considerado pequeno (270 indivíduos em média). Profundidade, correnteza, substrato, aliadas à concentração de detrito vegetal explicam melhor a variação nas densidades. Ações urgentes para conservação de E. vicentespelaea incluem a proteção das nascentes do Parque Estadual de Terra Ronca.

Orbital pacing and ocean circulation-induced collapses of the Mesoamerican monsoon over the past 22,000 y.

The dominant controls on global paleomonsoon strength include summer insolation driven by precession cycles, ocean circulation through its influence on atmospheric circulation, and sea-surface temperatures. However, few records from the summer North American Monsoon system are available to test for a synchronous response with other global monsoons to shared forcings. In particular, the monsoon response to widespread atmospheric reorganizations associated with disruptions of the Atlantic Meridional Overturning Circulation (AMOC) during the deglacial period remains unconstrained. Here, we present a high-resolution and radiometrically dated monsoon rainfall reconstruction over the past 22,000 y from speleothems of tropical southwestern Mexico. The data document an active Last Glacial Maximum (18-24 cal ka B.P.) monsoon with similar δ(18)O values to the modern, and that the monsoon collapsed during periods of weakened AMOC during Heinrich stadial 1 (ca. 17 ka) and the Younger Dryas (12.9-11.5 ka). The Holocene was marked by a trend to a weaker monsoon that was paced by orbital insolation. We conclude that the Mesoamerican monsoon responded in concert with other global monsoon regions, and that monsoon strength was driven by variations in the strength and latitudinal position of the Intertropical Convergence Zone, which was forced by AMOC variations in the North Atlantic Ocean. The surprising observation of an active Last Glacial Maximum monsoon is attributed to an active but shallow AMOC and proximity to the Intertropical Convergence Zone. The emergence of agriculture in southwestern Mexico was likely only possible after monsoon strengthening in the Early Holocene at ca. 11 ka.