Introduction
Recruitment from seeds following fire is a key factor for the maintenance of populations of many species with physically dormant seeds throughout the world (e.g. Auld and O'Connell, Reference Auld and O'Connell1991; Moreira and Pausas, Reference Moreira and Pausas2012; Ooi et al., Reference Ooi, Denham, Santana and Auld2014). Physical dormancy (PY), or seed coat impermeability to water (Rolston, Reference Rolston1978; Baskin and Baskin, Reference Baskin and Baskin2004; Finch-Savage and Leubner-Metzger, Reference Finch-Savage and Leubner-Metzger2006), is common in many ecosystems and in many plant families, but it is especially relevant in tropical Fabaceae (Baskin et al., Reference Baskin, Baskin and Li2000; Jayasuriya et al., Reference Jayasuriya, Wijetunga, Baskin and Baskin2013; Baskin and Baskin, Reference Baskin and Baskin2014). Although PY may have emerged as a response to distinct selective pressures rather than fire, such as drought and seasonality (Bradshaw et al., Reference Bradshaw, Dixon, Hopper, Lambers and Turner2011; Santana et al., Reference Santana, Baeza and Blanes2013; Willis et al., Reference Willis, Baskin, Baskin, Auld, Venable, Cavender-Bares, Donohue and Casa2014; Jaganathan, Reference Jaganathan2015; Jayasuriya et al., Reference Jayasuriya, Athugala, Wijayasinghe, Baskin, Baskin and Mahadevan2015), its alleviation under natural conditions has been suggested to be fire dependent in many fire-prone habitats (Auld and O'Connell, Reference Auld and O'Connell1991; Auld and Denham, Reference Auld and Denham2006; Keeley et al., Reference Keeley, Pausas, Rundel, Bond and Bradstock2011; Moreira and Pausas, Reference Moreira and Pausas2012; Ooi et al., Reference Ooi, Denham, Santana and Auld2014).
Nevertheless, daily temperature fluctuations may also play a role in PY alleviation in fire-prone ecosystems (Auld and Bradstock, Reference Auld and Bradstock1996; Santana et al., Reference Santana, Bradstock, Ooi, Denham, Auld and Baeza2010, 2013). Relatively high temperature fluctuations occur in post-fire vegetation due to increased solar irradiance (Auld and Bradstock, Reference Auld and Bradstock1996; Fidelis and Blanco, Reference Fidelis and Blanco2014), but temperature fluctuations also occur in undisturbed vegetation gaps (Santana et al., Reference Santana, Baeza and Blanes2013). On the other hand, there are many cases in which the temperature required to break PY is higher than those reached in vegetation gaps, and thus fire passage would be necessary to break dormancy (Moreira and Pausas, Reference Moreira and Pausas2012). PY has been reported to be broken at different temperature thresholds, and these data have been used to classify species into functional groups according to their fire dependency: fire-obligate or fire-facultative, depending on the temperatures required to break PY (Ooi et al., Reference Ooi, Denham, Santana and Auld2014).
Determination of the temperature thresholds related to PY alleviation is crucial to disentangling the role of fire and temperature fluctuations as germination cues in fire-prone environments (Moreira and Pausas, Reference Moreira and Pausas2012; Ooi et al., Reference Ooi, Denham, Santana and Auld2014), and it is also important to clarify seed tolerance to fire-related temperatures (Jaureguiberry and Díaz, Reference Jaureguiberry and Díaz2015; Ribeiro et al., Reference Ribeiro, Barbosa, van Langevelde and Borghetti2015). Moreover, it is necessary to determine such temperature thresholds from a field perspective (e.g. Santana et al., Reference Santana, Baeza and Blanes2013). Therefore, if PY break is fire dependent, one should expect dormancy to be alleviated only at temperatures higher than those found in daily temperature fluctuations at the soil surface (Moreira and Pausas, Reference Moreira and Pausas2012; Ooi et al., Reference Ooi, Denham, Santana and Auld2014).
The question regarding fire-mediated PY break has been mainly addressed in Australia (e.g. Auld and O'Connell, Reference Auld and O'Connell1991; Knox and Clarke, Reference Knox and Clarke2006; Scott et al., Reference Scott, Setterfield, Douglas and Andersen2010; Ooi et al., Reference Ooi, Denham, Santana and Auld2014) and Mediterranean vegetation (e.g. Herranz et al., Reference Herranz, Ferrandis and Martínez-Sánchez1998; Reyes and Trabaud, Reference Reyes and Trabaud2009; Moreira et al., Reference Moreira, Tormo, Estrelles and Pausas2010; Santana et al., Reference Santana, Baeza and Blanes2013). In the Cerrado, few data are derived from field experiments (but see Hoffmann, Reference Hoffmann2000; Dodonov et al., Reference Dodonov, Xavier, Tiberio, Lucena, Zanelli and Matos2014) and most data obtained from laboratory studies suggest that fire-related heat shock does not break PY (Ribeiro et al., Reference Ribeiro, Barbosa, van Langevelde and Borghetti2015; Fichino et al., Reference Fichino, Dombrovski, Pivello and Fidelis2016; Zupo et al., Reference Zupo, Baeza and Fidelis2016). Therefore, we still lack a comprehensive idea of the overall effects of fire on dormancy alleviation and seed germination in grassy biomes, which have been typically neglected (Parr et al., Reference Parr, Lehmann, Bond, Hoffmann and Andersen2014). Such a field-related perspective should help us to understand germination responses to fire in the Neotropical savannas, such as the open Cerrado formations (campo sujo; Coutinho, Reference Coutinho, Huntley and Walker1982). The Cerrado is a Neotropical complex of open and closed savannas (Furley, Reference Furley1999; Oliveira-Filho and Ratter, Reference Oliveira-Filho, Ratter, Oliveira and Marquis2002), where fire has been present for at least four million years (Simon et al., Reference Simon, Grether, Queiroz, Skema, Pennington and Hughes2009).
Our purpose was to evaluate different scenarios for seed germination and survival from a field perspective, aiming to disentangle the role of fire-related and non-fire-related germination cues in a Neotropical savanna. Thus we carried out three field experiments with legume shrub seeds from Cerrado open savannas, according to where seeds could be located in/on the soil. Specifically, we tested the effects of (1) fire on exposed seeds (in the upper layer of the soil), (2) fire on buried seeds and (3) temperature fluctuations under non-fire-related conditions on dormancy break and maintenance of seed viability.
Additionally, we addressed the following hypotheses. (1) As recurrent Cerrado fires consume up to 90% of the grassy fuel load (Coutinho, Reference Coutinho, Huntley and Walker1982; Kauffman et al., Reference Kauffman, Cummings and Ward1994; Miranda et al., Reference Miranda, Sato, Neto, Aires and Cochrane2009), we expected fire to kill most of the seeds located on the soil surface, as reported for other fire-prone ecosystems (Carrington, Reference Carrington2010; Dayamba et al., Reference Dayamba, Savadogo, Zida, Sawadogo, Tiveau and Oden2010). (2) Below-ground soil heating during fires could be increased by a higher amount of fuel load (Choczynska and Johnson, Reference Choczynska and Johnson2009; Gagnon et al., Reference Gagnon, Harms, Platt, Passmore and Myers2012, 2015), which in this case is the amount of live and dead grassy biomass, so we expected fires to have a positive effect on seed germination of buried seeds at increased fuel load conditions. (3) Natural temperature fluctuations, especially in vegetation gaps, could alleviate PY in the Cerrado, as reported for Australian legumes (Santana et al., Reference Santana, Bradstock, Ooi, Denham, Auld and Baeza2010) and Mediterranean Basin obligate seeders (Santana et al., Reference Santana, Baeza and Blanes2013).
Materials and methods
Study site and seed collection
Three separate field experiments (Table 1) were carried out at the Reserva Natural Serra do Tombador, in Central Brazil (47°45′–51′W and 13°35′–38′S, 8900 ha, 560–1118 m above sea level). The area has been subjected to natural and anthropogenic fires, with a mean return interval of 3 years (Daldegan et al., Reference Daldegan, Carvalho Júnior, Guimarães, Gomes, Ribeiro and McManus2014). The climate has a marked dry season from May to September (total precipitation during this period <60 mm) and a wet season from October to April, when most of the annual precipitation (1300–1500 mm/year) occurs. Annually, mean temperatures range from 22 to 25°C and September is usually the hottest month. Minimum temperatures may be <15°C and maximum temperatures up to 36°C (Fundação Grupo Boticário, 2011). Vegetation is predominantly campo sujo, which is an open savanna dominated by a species-rich herbaceous layer with scattered shrubs and small trees (Coutinho, Reference Coutinho, Huntley and Walker1982).
PY, physical dormancy; ND, non-dormant.
We collected seeds from four leguminous shrub species commonly found in the area: Mimosa leiocephala Benth., Harpalyce brasiliana Benth., Senna corifolia (Benth.) H.S. Irwin and Barneby, and Bauhinia dumosa Benth. (Table 1). Seeds from all species were collected from several individuals (n > 10) and stored at 5°C for up to 1 year until the beginning of the experiments. All species had physically dormant seeds (Table 1), except B. dumosa, which has permeable seed coats (Zupo et al., Reference Zupo, Baeza and Fidelis2016).
Fire effects on exposed seeds
We evaluated fire effects on survival of exposed seeds by carrying out experimental fires with seeds placed in the upper soil layer. The experiment was performed in July 2014 (mid-dry season), a period in which the study species are shedding seeds (authors’ personal observation) and when most anthropogenic fires occur in the Cerrado (Ramos-Neto and Pivello, Reference Ramos-Neto and Pivello2000; Miranda et al., Reference Miranda, Sato, Neto, Aires and Cochrane2009). We avoided patches invaded by Urochloa brizantha, an invasive African grass species, because it can influence fire parameters (Gorgone-Barbosa et al., Reference Gorgone-Barbosa, Pivello, Bautista, Zupo, Rissi and Fidelis2015).
Seeds were placed in experimental plots subjected to fires (Fig. 1). We independently burned four distinct plots (15 × 20 m, excluded from fire for 2 years), which were located at least 20 m from each other. Seeds were placed in aluminium dishes (7 cm diameter × 0.5 cm deep) filled with local soil and positioned on the soil surface. Seeds were carefully placed within the aluminium dishes, so that they would have at least part of their seed coat exposed directly to fire. Three aluminium dishes were placed under the native vegetation (grass tussocks) in each plot (3 dishes × 4 plots = 12 samples). We conducted head fires (wind direction), and fires were set in the morning for safety reasons (Whelan, Reference Whelan1995); all plots were burned in the same week. Fire temperatures were recorded every 2 s with type K thermocouple sensors attached to data loggers (Novus LogBox). We calculated fire residence times at temperatures ≥60°C, which is a standardized temperature threshold lethal for plant tissue (Daniell et al., Reference Daniell, Chappell and Couch1969; Dayamba et al., Reference Dayamba, Savadogo, Zida, Sawadogo, Tiveau and Oden2010). Additionally, we calculated residence time of fire temperatures ≥100°C, a threshold easily reached by fire under exposed conditions. The number of seeds per dish varied between species due to constraints in seed availability (see Table 1). Control seeds were transported to the field and kept stored in thermal bags at room temperature, thus not heated. After fires, both control and treatment seeds were tested for germination in the laboratory (see germination procedures below).
Fire effects on buried seeds
To test the effects of fire on the survival and germination of buried seeds, we used seeds of two species with different traits in relation to seed coat permeability: one with impermeable-coated seeds (PY, M. leiocephala) and the other with permeable seeds (non-dormant, B. dumosa, see Table 1). Since the amount of fuel (live and dead grassy species) can influence both fire intensity and temperatures reached during fires (Gagnon et al., Reference Gagnon, Passmore, Slocum, Myers, Harms, Platt and Paine2015; M.N. Rissi et al., unpublished data), we manipulated the fuel load to assess the effects of doubling the amount of above-ground biomass on soil heating and thus on seed germination and survival of buried seeds. Therefore, the following treatments were carried out in the field: (1) no manipulation of fuel load (~700 g m–2) and (2) increased fuel load by adding 700 g m–2 of biomass collected from neighbouring plots to double the fuel load. For this treatment, four 30 × 30 m plots were individually burned, and we established three subplots (2 × 2 m) for each biomass manipulation treatment within each plot (3 subplots × 4 plots = 12 subplots/treatment). In each subplot, we placed an aluminium dish with 10 seeds/species buried 1 cm below ground (Fig. 1; Table 1). Fires were set in October 2015 (late-dry season), using experimental procedures similar to those described above, and fire temperatures were recorded (type K thermocouple sensors attached to data loggers) every 2 s at 1 cm below ground in each subplot/treatment. However, measurements in most sensors at the increased fuel load treatment failed and therefore they are not presented in detail. Control seeds were transported to the field, but kept stored at room temperature, and after fires both control and treatment seeds were tested for germination in the laboratory (see below).
Temperature fluctuation effects
We used seeds of the four species at two different field treatments to test the effects of temperature fluctuations on seed germination: (1) shaded: seeds placed under native grass tussocks; and (2) gap: seeds placed in bare soil gaps. The soil-filled aluminium dishes (0.5 mm deep) with seed samples were placed at soil level in shade or in a gap in the field for ca 75 days from July to October (dry season). Soil temperatures were recorded every 30 min by sensors coupled to data loggers. The sensors were placed at the soil surface in each treatment, near the aluminium dishes: in the shaded treatment, sensors were placed under tussocks of native grasses; and in the gap treatment they were exposed to sunlight. The treatments were applied in four unburned plots and followed the same experimental design as described above (3 dishes × 4 plots = 12 samples/treatment; Fig. 1; Table 1). After 75 days, treatment and control (stored at room temperature) seeds were tested for germination, as described below.
Germination tests after field treatments
Upon the completion of the field treatments, seeds were packed in thermal bags and immediately transported to the laboratory. Treatment and control seeds were then placed in Petri dishes (60 mm diameter) with a double layer of filter paper saturated with distilled water and set to germinate in germination chambers at 27°C (12 h of light); the average temperature was recorded at soil level in the study site and in accordance with other studies performed with Cerrado seeds (Fichino et al., Reference Fichino, Dombrovski, Pivello and Fidelis2016). We used a constant temperature to avoid possible additional effects of alternating temperature in seed germination. Seeds were considered germinated when exhibiting radicle protrusion (Bewley et al., Reference Bewley, Bradford, Hilhorst and Nonogaki2013) and germination was recorded three times a week for four consecutive weeks.
At the end of the germination tests, non-germinated seeds were scarified, allowed to imbibe and then cut and tested for the viability using tetrazolium solution (1%, buffer pH 7). Seeds with embryos that stained red were considered to be viable, and those with non-stained embryo or those that were visibly burned or showed flaccid tissues were considered to be dead (Lakon, Reference Lakon1949).
Data analyses
All our experiments followed a similar experimental design (Fig. 1), with the seed samples nested within the experimental plots (3 dishes × 4 plots = 12 samples/species/treatment). Therefore, we performed generalized linear mixed models (GLMMs) with a binomial distribution (see Santana et al., Reference Santana, Baeza and Blanes2013) to separately evaluate: seed germination (binary data considering that a seed could germinate or not) and seed viability (a seed could be viable or not at the end of the trials). As the dishes were nested within the plots, they were considered as the random effects in the analyses. The field treatments (fire treatments or shaded/gap temperature fluctuations, as well as their respective controls) were treated as fixed effects. The controls were considered as the baseline for the intercept in the models. Models were fitted for each species separately in each experiment. Post hoc Tukey's tests were performed to evaluate multiple comparisons among treatments. All analyses were performed using the packages lme4 (Bates et al., Reference Bates, Maechler, Bolker and Walker2015) and multcomp (Hothorn et al., Reference Hothorn, Bretz and Westfall2008) in R software 3.2.5 (R Core Team, 2016) and significance was determined with α = 0.05.
Results
Fire effects on exposed seeds
Maximum fire temperatures were 225 ± 152°C, with residence time of temperatures ≥60°C equal to 80 ± 26 s and ≥100°C always less than 1 min. For M. leiocephala, germination decreased from 26 ± 9% (control) to 9 ± 7% [fire treatment, P = 0.002; Table 2 (a); Fig. 2A]. Germination of H. brasiliana and S. corifolia was nearly null in both the control and the fire exposure treatments [Table 2 (a); Fig. 2A]. However, for B. dumosa, a species with permeable seeds, fire exposure reduced germination from 88 ± 4 to 11 ± 22% [(P < 0.001); Table 2 (a); Fig. 2A]. Initial seed viability ranged from 63% (H. brasiliana) to 90% (B. dumosa), and seed viability of all four species decreased after fire exposure to less than 30% [all (P < 0.001); Table 2 (a); Fig. 2B].
Significant P-values (≤0.05) are highlighted in bold.
Fire effects on buried seeds
Below-ground temperatures reached mean maxima of 54 ± 14°C, and thus they did not exceed the threshold of 60°C for residence time calculations in the unmanipulated treatment. Sensors failed to measure below-ground temperatures in the increased fuel load condition, however; recordings of fire temperatures in the same area point out that mean maxima temperatures reach around 80°C at 1 cm depth in sites under high biomass accumulation (see Discussion).
Regarding seed germination, there was no difference in germination percentage of M. leiocephala seeds between the control (5 ± 4%) and the unmanipulated treatment [3 ± 5%, Table 2 (b); Fig. 3A]. Moreover, the increased fuel load treatment had a positive effect on seed germination of M. leiocephala, resulting in a 6-fold increase in germination [P = 0.011; Table 2 (b); Fig. 3A]. There was no difference in seed viability among treatments for this species [Table 2 (b)], which was over 70% for all treatments (Fig. 3B). For B. dumosa seeds, both seed germination and viability percentages were not affected by the treatments [Table 2 (b)], remaining ≥88% (Fig. 3A and B).
Temperature fluctuation effects
Soil temperature under the shaded condition ranged from 20 to 38°C (Fig. 4) and had little or no effect on seed germination for any species [Table 2 (c); Fig. 5A]. On the other hand, soil temperature in gaps ranged from 18 to 53°C and remained ≥50°C for at least 2 h each day (Fig. 4).
Temperature fluctuations in the gap treatment had a positive effect in alleviating PY in M. leiocephala (P < 0.001) and H. brasiliana [P = 0.001; Table 2 (c)]. For M. leiocephala, the gap condition enhanced germination percentage (58 ± 17%) in relation to both shaded treatments (16 ± 4%) and the control (26 ± 9%; Fig. 5A). For H. brasiliana, the gap condition increased germination to 20 ± 5% compared with the control (5 ± 3%, Fig. 5A). However, none of the treatments alleviated dormancy in S. corifolia seeds [Table 2 (c); Fig. 5A]. Seeds of B. dumosa were negatively affected by temperature fluctuation in the gaps [P < 0.001; Table 2 (c); Fig. 5A].
Seed viability of all species in the shaded treatment did not differ from their respective controls [Table 2 (c); Fig 5B]. Nonetheless, the gap treatment had a negative effect on seed viability from 20 to 30% across species [Table 2 (c); Fig. 5B].
Discussion
There is an ongoing debate on the relative importance of fire-related temperatures vs daily temperature fluctuations in alleviating PY in fire-prone ecosystems (Moreira et al., Reference Moreira, Tormo, Estrelles and Pausas2010; Santana et al., Reference Santana, Bradstock, Ooi, Denham, Auld and Baeza2010, 2013; Ooi et al., Reference Ooi, Denham, Santana and Auld2014), and our study helps to disentangle these germination cues from a field perspective in a Neotropical savanna. Theoretically, PY should be broken at different temperature thresholds, so dormancy alleviation could be classified as being fire related or not (Moreira and Pausas, Reference Moreira and Pausas2012; Ooi et al., Reference Ooi, Denham, Santana and Auld2014). However, we argue that Cerrado leguminous seeds have their PY (or at least part of it) alleviated by two different mechanisms: (1) during hotter fires, if seeds are stored in the soil, or (2) when exposed to daily temperature fluctuations.
Although not tested under the buried conditions in our field experiments, some seeds of H. brasiliana have part of their PY alleviated after heat shocks applied in the laboratory (H.L. Zirondi et al., unpublished data). Therefore, seeds of both M. leiocephala and H. brasiliana should be classified as facultative regarding their functional responses to fire (see Ooi et al., Reference Ooi, Denham, Santana and Auld2014). PY of S. corifolia seeds, on the other hand, was neither alleviated from laboratory heat shocks (data not shown) nor from the enhanced field temperature fluctuations, which could suggest that these legume seeds have other habitat-specific dormancy-breaking mechanisms under natural conditions, perhaps related to wetter conditions (van Klinken and Goulier, Reference van Klinken and Goulier2013).
Fire effects on exposed seeds caused a high mortality, as reported for most seeds throughout the world when placed in the upper layer of the soil (Auld and O'Connell, Reference Auld and O'Connell1991; Bradstock and Auld, Reference Bradstock and Auld1995; Carrington, Reference Carrington2010; Dayamba et al., Reference Dayamba, Savadogo, Zida, Sawadogo, Tiveau and Oden2010). However, seeds buried in the soil would be insulated and could have PY alleviated, as reported for Australian leguminous seeds (Auld and O'Connell, Reference Auld and O'Connell1991; Bradstock and Auld, Reference Bradstock and Auld1995). Conversely, below-ground temperatures required for PY break seem to be only reached under more intense fires (Knox and Clarke, Reference Knox and Clarke2006). Despite that, Cerrado fires are mostly fast and below-ground soil heating is usually negligible (~50°C; Miranda et al., Reference Miranda, Miranda, Dias and Dias1993), with minor consequences to the seed bank (Andrade and Miranda, Reference Andrade and Miranda2014).
Nevertheless, hotter fires may occur in the Cerrado when the return intervals take 4 years or more, due to a substantial accumulation of fuel load (Coutinho, Reference Coutinho, Huntley and Walker1982), which would also enhance below-ground fire temperatures, as reported for other high-diversity flammable communities (e.g. Gagnon et al., Reference Gagnon, Passmore, Slocum, Myers, Harms, Platt and Paine2015). In our study area, previous measurements of fire temperatures 1 cm below ground in plots with 4 years of fuel load accumulation, detected temperatures reaching ≥60°C for about 3 min, occasionally recording temperatures ≥100°C (mean maxima = 80°C; maximum observed = 154°C; T. Zupo et al., unpublished data). On the other hand, anthropogenic fires have been suggested to change fire regimes in Cerrado open savannas, by shifting season of occurrence from wet to the dry season and shortening the frequency of return (Ramos-Neto and Pivello, Reference Ramos-Neto and Pivello2000; Miranda et al., Reference Miranda, Sato, Neto, Aires and Cochrane2009).
Fire-stimulated germination traits should not have been favoured in fire-prone systems that undergo surface fires (Bond and Midgley, Reference Bond and Midgley2003; Bradshaw et al., Reference Bradshaw, Dixon, Hopper, Lambers and Turner2011), such as the open savannas where fire episodes are frequent and less severe (Bond and Keeley, Reference Bond and Keeley2005). Although there has been no evidence of fire-stimulated germination from laboratory experiments (Le Stradic et al., Reference Le Stradic, Silveira, Buisson, Cazelles, Carvalho and Fernandes2015; Ribeiro et al., Reference Ribeiro, Barbosa, van Langevelde and Borghetti2015; Fichino et al., Reference Fichino, Dombrovski, Pivello and Fidelis2016; Zupo et al., Reference Zupo, Baeza and Fidelis2016), we argue that fire-related conditions can potentially break PY, as was observed in at least 30% of M. leiocephala buried seeds under increased fuel load conditions. Therefore, fire could play a role in seed recruitment for a proportion of seeds from the Cerrado soil seed bank.
Fire also has been recognized as having an indirect effect on PY alleviation by removing vegetation and consequently increasing daily temperatures at upper soil layers (~0.5 cm), therefore reaching temperature thresholds required for gap-dependent seeds to break PY (Ooi et al., Reference Ooi, Denham, Santana and Auld2014), which do not seem to occur in vegetated sites (Auld and Bradstock, Reference Auld and Bradstock1996; Santana et al., Reference Santana, Bradstock, Ooi, Denham, Auld and Baeza2010). However, gaps in unburned sites seem to have the same effect in seedling recruitment, suggesting that biomass removal, which increases the daily temperature fluctuations, plays a role in regeneration from seeds irrespective of fire (Santana et al., Reference Santana, Baeza and Blanes2013).
Previous laboratory simulations of temperature fluctuations had already recognized a decrease in germination in the permeable-coated B. dumosa seeds, but such experiments had no effect on PY alleviation of M. leiocephala (Zupo et al., Reference Zupo, Baeza and Fidelis2016). Instead, our results show that temperature fluctuation in gaps enhanced germination for M. leiocephala and H. brasiliana seeds, even though PY was not fully alleviated. Thus, from a field perspective, vegetation gaps provide an important micro-environment with higher temperature fluctuations that could lead to the alleviation of PY in legume seeds, enabling their germination in both post-fire environments (where temperature fluctuations will be higher due to the removal of the above-ground vegetation), as well as in fire-free intervals if seeds reach such gaps.
PY release has not yet been fully explained for Cerrado open savannas. Our four study species are dominant in their plant community, and distinct traits related to dormancy relief and germination strategies could explain a diversity of regeneration niches and species co-existence (see Grubb, Reference Grubb1977). Therefore, other species-specific processes may be related to releasing PY in these species. Further studies are warranted to understand if water availability could play any role coupled with daily heating temperatures (Moreno-Casasola et al., Reference Moreno-Casasola, Grime and Martínez1994; van Klinken et al., Reference van Klinken, Flack and Pettit2006), and if seeds could become sensitive to dormancy-breaking conditions as they age in soil seed banks (van Assche et al., Reference van Assche, Debucquoy and Rommens2003; Jayasuriya et al., Reference Jayasuriya, Baskin and Baskin2009; Gama-Arachchige et al., Reference Gama-Arachchige, Baskin, Geneve and Baskin2012; Liyanage and Ooi, Reference Liyanage and Ooi2017).
This was the first attempt to test fire- and non-fire-related cues of seed germination within an experimental field approach for the Cerrado open savannas. We draw three main conclusions from our experiments: (1) most seeds die when exposed directly to fire; (2) PY could be alleviated during hotter fires when seeds were buried, and thus stored in the soil seed bank; and (3) daily temperature fluctuations in gaps also break PY in seeds of some species on the soil surface, and thus many seeds may germinate or die instead of being incorporated into the soil seed banks.
Acknowledgements
We thank the fire team from the Reserva Natural Serra do Tombador: A.F. Terra, G.A. Berberino, R.B. de Almeida and S.A. Borges. We also thank E. Gorgone-Barbosa, M.N. Rissi and M.B. Cunha for the collaboration in field work. The first author holds a scholarship from Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES). This study was funded by Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP 2015/06743-0), Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq 455183/2014-7) and Fundação Grupo Boticário (0153_2011_PR; 0106_2011_PR). F.A.O. Silveira (482720/2014) and A. Fidelis (306170/2015-9) received research grants from CNPq.